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District Survey Report Mahasamund AS PER NOTIFICATION NO. S.O. 141(E) NEW DELHI, 15TH JANUARY, 2016 OF MINISTRY OF ENVIRONMENT, FOREST AND CLIMATE CHANGE 2016 DGM [Type the company name] 27/05/2016 DIRECTORATE OF GEOLOGY AND MINING MINERAL RESOURCES DEPARTMENT Govt. of Chhattisgarh
Transcript

District Survey Report Mahasamund

AS PER NOTIFICATION NO. S.O. 141(E) NEW DELHI, 15TH JANUARY, 2016 OF MINISTRY OF ENVIRONMENT, FOREST AND CLIMATE CHANGE

2016

DGM[Type the company name]

27/05/2016

DIRECTORATE OF GEOLOGY AND MININGMINERAL RESOURCES DEPARTMENT

Govt. of Chhattisgarh

1

LOCATION AND COMMUNICATION MAP – MAHASAMUND DISTRICT

2

1.Introduction

Mahasamund district is situated in the Eastern part of the Chhattisgarh state. It falls in the Survey of India’s Degree Sheet No. 64 K,O,L and G between the Latitude 20º49’30” : 21º33’07”N and Longitude 81º59’56”:83º16’10” E.t The district is bounded by Raipur district in the north,west and southwest, Raigarh district in the north-east, Kalahandi and Sambalpur dist. Of Orissa state in the south-east,south and east.

Mahasamund district came into being in July 1998. It is famous for its traditional background. The region once capital of South Kosala ruled by ‘Somyavansiya Empores’ Mahasamund district is spread out in an area of 4790 sq.km in the Central-East of Chhattisgarh state.Total forest cover of the area is 1101.99 sq.km as per 2010-2011 data. District includes 05 tahsil and 1145 villages.

Headquarter Mahasamund is located in the south-west corner of the districtwith Pithoura,Saraypali, Bagbahra and Basana are the tahsil of the districtLocated on the East Coast Railway Zone.and Mahasamund district has three National Highway which are NH 53 (Nagapur-Sambalpur), NH 217 and NH 216, most of the destinations are well connected with tar roads in the district.

District survey report has been prepaired as per notification No. S.O. 141 (E) New Delhi,15 January,2016 of Ministry of Environment,Forest and Climate Change.

The report primarily is focused on the Geological Details i.e. minerals its occurrence, deposit and mining activity, along with the mineral production and royalty details, geographical and infrastructure information is also included.

District Environment Impact Assessment Authority and District Environment assessment committee will utilize this report in favour of the environment concerned activities and act accordingly.

Also this report will act as reference for the lease holders of minerals and those willing to apply for lease.

3

2. Overview of Mining Activity in the District

Mahasamund is important district for minor minerals. These minerals are Quartz, Quartzite, Granite, Limestone, Flag stone, Sand, Soiland Laterite. Occurance of Molybdenum and Flourite are also reported in veins and veinlets in Sheard zone. Quartzite is reported in Chourakhuta and Makarmuta village.

About 100 quarry leases have been given for flag stone at villages Barbaspur, Ghodari, Nandgaon, Belsonda, Achholi, Mudhena, Nisda, Paragaon etc. 18 granite quarry leases allotted asordanary stone mining in which is not suitable for cutting and polishing in villages Banskonda, Rengadih, Rampur, Laxmipur, Kishanpur, Tilganpur, Chuipali, Chirraleva, Dhaman ghutkur, Chuhiya etc., 11 quarry lease for soil have given at Barbaspur, Ghodari, Nandgaon, Mudhena, Lafinkhurd, Belsonda, Achholi, Bamhani villages etc., 2 granite leases allotted forstone crusher at Hadaband, 7 Quartz lease given at villages Udela, Khursipahar, Salhetarai, Koliyaridih, Patparpali, Chhindoli, Khogasa etc., One fireclay lease at Benardih village.

8 ratghat (sand) on the bank of Mahanadi and Jonk riverhave been leased out at different villages for sand miningto Panchayat.

Approximately in 2015-16 Rs. 6,86,79,281is earned forall minor minerals.

State Government is carrying on various infrastructure development project in all district, like Pachri Nirman, Dams, Over bridge on rivers/nala, approach road etc., all above works require Sand in different sizes which is in huge demand.

3. List of Mining Leases and Sand in the District with location, area and period of validity

(ii) List of Quary lease in the district with location area and period of validity

Sno

Name of the

lessee

address of the lesse

Date of applicant

on.

Number and date of grant

date of executi

on

period mineral/

mineral

Name of the village

Name of

Gram Panchayat

Name of the

Block

khasra No.

total area (in

Hect.)

cordinates and toposheet no. (if available

Date and

period of

renewal/Extensio

n

Date of

transfer, if any and the

name and

address of the

transferee

No. and Date of approval of

QP/SOM,

annual approved quantity & period

No. and Date of EC and

annual approved

quantity

Remark

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19

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34

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panzkdj

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&&^^&&^^&&

44

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Q'khZiRFkj

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45

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17.10.05894/

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11.07.16

Q'khZiRFkj

vNksyh vNksyh egkleqan950,951,956

0.7 NA 10.7.15

&&^^&&^^&&

46

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Lo- Jh jked`".k vxzoky

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rglhy o ftyk jk;iqj

30.7.051530/

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15.11.06 to

14.11.16

Q'khZiRFkj vNksyh vNksyh egkleqan

1815,1816,18171820

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47

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16.4.08 to15.4.1

8

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48

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Q'khZiRFkj

ukanxkoa ukanxkao egkleqan 2753 0.25 NA 24.12.16

Lo- Jh ujs'k

panzkdj fuoklh ukanxkao ftyk egkleqa

n

&&^^&&^^&&

49

Jh rkfjd eqchu

dqjS'kh vk0 Jh eqchu vegn dqjS'kh

cSju cktkj jk;iqj ftyk jk;iqj

19.7.073733/

23.10.0724.10.07

23.10.07 to

22.10.17

iRFkj dzs'kj

ckaldwMkckaldwM

k egkleqan

300,302,303

1.07 NA 21.10.16

&&^^&&^^&&

50

Jh jke'kj.k VaMu vk0 Jh fM/kk: jke VaMu

xzke fcjdksuh rglhy o ftyk

egkleqan

19.1.072051/

4.10.0819.11.08

4.10.08 to

3.10.18

pwukiRFkj

cjcliqjcjcliq

jegkleqan 311 0.4 NA 02.10.

2017

&&^^&&^^&&

51

Jh vuqie vxzoky vk-

Lo- Jh jked`".k vxzoky

iqjkuh cLrh jk;iqj

rglhy o ftyk jk;iqj

14.1.09363/

3.2.0912.2.09

28.1.09 to

27.1.19

Q'khZiRFkj

csylksaMkcsylksaM

kegkleqan 235 0.9 NA 26.1.1

8

Jherh ok.kh frokjh ifr Jh y{ehdka

r frokjh fuoklh csylks.Mk

ftyk egkleqa

n

&&^^&&^^&&

52

es-ch-,l-lh-ih-,y- fy-izks- Jh th-,l-ds-jko

gky eqdke ?kksMkjh

rglhy o ftyk

egkleqqn

22.12.08480/

16.2.0921.1.09

15.1.09 to

14.1.19

Q'khZiRFkj

cjcliqj cjcliqj

egkleqan 177 2.4 NA 13.1.2018

Jh vt; panzkdj vk-Jh eugj.k panzkdj fuoklh cjcliq

j rglhy o ftyk

&&^^&&^^&&

9

egkleqqan

53

Jh rstdqekj

dqjsZ vk0 Jh ghjk/kj dqjsZ

xzke cklhu rglhy o ftyk

egkleqan

17.9.08210/

19.1.0921.1.09

15.1.09 to

14.1.19

Q'khZiRFkj

vNksyh vNksyh egkleqan 14 0.4 NA 2.10.08

&&^^&&^^&&

54

Jh jke'kj.k VaMu vk0 Jh fM/kk: jke VaMu

xzke fcjdksuh rglhy o ftyk

egkleqan

17.7.062052/

4.10.0819.11.08

4.10.08 to

3.10.18

Q'khZiRFkj

cjcliqj cjcliqj

egkleqan 358 0.2 NA 2.10.17

&&^^&&^^&&

55

Jh vfer panzkdj vk0 Jh ukjn panzkdj

egkleqan rglhy o ftyk

egkleqn

30.6.082040/

3.10.0815.10.08

3.10.08 to

2.10.18

Q'khZiRFkj ukanxkoa ukanxkao egkleqan

2649,2650,2659,

0.14 NA 1.10.18

Jh vej flag vk-Jh Hkkjr flag

fuoklh egkleqa

n

&&^^&&^^&&

56

Jh txUukFk lkgw vk0

Jh fclsyky lkgw

xzke fcjdksuh rglhy o ftyk

egkleqan

7.12.0101615/

23.8.01130.8.201

1

30.8.11 to

29.8.16

Q'khZiRFkj

vNksyh vNksyh egkleqan

1750,1751,1753,1754,1756,1757,

0.2 NA 28.8.15

&&^^&&^^&&

57

Jh vuqie vxzoky

iqjkuh cLrh jk;iqj

rglhy o ftyk jk;iqj

16.7.092490/

9.11.0919.11.09

6.11.09 to

5.11.19

Q'khZiRFkj

vNksyh vNksyh egkleqan

1405/2 1407140414091276

2 NA 13.11.15

&&^^&&^^&&

10

5

Jh yfyr fu"kkn vk0 Jh dfiy fu"kkn

'kadj [knku dke-lg-lfe-eq<suk

rglhy o ftyk

egkleqan

11.8.072070/

7.10.086.10.08

6.10.08 to

5.10.18

pwukiRFkj

eq<suk eq<suk egkleqan 330 0.3 NA 4.10.17

&&^^&&^^&&

59

Jh fofiu dqekj tSu vk0 Jh /kjepan tSu

uokikjk jkfte rglhy vHkuiqj ftyk jk;iqj

27.12.08981/

20.5.091.6.09

1.6.09 to

31.5.19

Q'khZiRFkj

vNksyh vNksyh egkleqan

779/1,2778,

758/2759760,761

0.8 NA 30.5.15

&&^^&&^^&&

60

Jh vej flag vk0 Lo0 Jh

Hkkjr flag

egkleqan rglhy o ftyk

egkleqn

3.1.09938/

19.5.0922.5.09

18.5.09 to

17.5.19

Q'khZiRFkj

?kksMkjh ?kksMkjh egkleqan 6 0.64 NA 16.5.18

&&^^&&^^&&

61

Jh pUnzgkl panzkdj vk0 Lo0

Jh jkef[kykou

egkleqan rglhy o ftyk

egkleqn

3.1.09931/

19.5.0922.5.09

18.5.09 to

17.5.19

Q'khZiRFkj ?kksMkjh ?kksMkjh egkleqan 346 0.5 NA 16.5.1

8

&&^^&&^^&&

62

Jh jkds'k dqekj

dkslys vk0 Jh esgr: dkslys

xzke ?kksMkjh rglhy o ftyk

egkleqan

14.1.091047/

25.5.0930.6.09

20.5.09 to

19.5.19

Q'khZiRFkj

?kksMkjh ?kksMkjh egkleqan 10 0.15 NA 18.5.2018

&&^^&&^^&&

63

Jh bnzlsu HkkaMsdj vk0 Jh uanwjke HkkaMsadj

jkfte rglhy jkfte ftyk jk;iqj

23.6.081049/

25.5.093.6.09

20.5.09 to

19.5.19

Q'khZiRFkj

cjcliqjcjcliq

jegkleqan 226 0.25 NA 18.5.2

018

Jh f'ko dqekj jk=s vk-

Jh lqdqy jk=s

fuoklh ?kksMkjh rglhy o ftyk egkleqa

n

&&^^&&^^&&

11

64

Jh v:.k dqekj vk0 Jh ikaMsjke

xzke ?kksMkjh rglhy o ftyk

egkleqan

23.5.08685/

3.3.0919.5.09

27.2.09 to

26.2.19

Q'khZiRFkj

?kksMkjh ?kksMkjh egkleqan 10 0.16 NA 25.2.2018

&&^^&&^^&&

65

Jh fnus'oj panzkdj vk0 Jh

useu yky panzkdj

xzke fcjdksuh rglhy o ftyk

egkleqan

13.4.09962/

20.5.0925.5.09

19.5.09 to

18.5.19

Q'khZiRFkj

?kksMkjh ?kksMkjh egkleqan 108 0.29 NA 17.5.18

&&^^&&^^&&

66

ujsUnz dqekj lq;Zoa'kh

jkfte rglhy jkfte ftyk jk;iqj

17.10.082128/ 7.7.09

25.7.091.7.09

to 30.6.19

Q'khZiRFkj

vNksyh vNksyh egkleqan 1885 0.45 NA 29.6.2018

&&^^&&^^&&

67

Jh vksedkj lq;Zoa'kh vk0 Jh jkeyky lq;Zoa'kh

jkfte rglhy jkfte ftyk jk;iqj

15.9.111338/

13.6.0129.7.2012

9.7.12 to

8.7.17

Q'khZiRFkj vNksyh vNksyh egkleqan 1406 0.18 NA 7.7.20

16

&&^^&&^^&&

68

Jh nhi dqekj vxzoky vk0 Lo0

Jh jkefuokj.k vxzoky

xzke ?kksMkjh rglhy o ftyk

egkleqan

14.5.092575/

16.9.0923.9.09

14.9.09 to13.9.1

9

Q'khZiRFkj

?kksMkjh ?kksMkjh egkleqan 95/1 2.7 NA 12.9.18

&&^^&&^^&&

69

Jh fot; panzkdj vk0 Jh ukjn jke panzkdj

egkleqan rglhy o ftyk

egkleqn

22.2.082340/

24.10.0928.10.09

24.10.09 to

23.10.19

Q'khZiRFkj

?kksMkjh ?kksMkjh egkleqan 10 0.8 NA 22.10.18

Jh vej flag vk-Jh Hkkjr flag

fuoklh egkleqa

n

&&^^&&^^&&

70

Jh vuqie vxzoky vk-

Lo- Jh jked`".k vxzoky

iqjkuh cLrh jk;iqj

rglhy o ftyk jk;iqj

3.3.092193/

22.10.0927.10.09

20.10.09

to19.10.19

Q'khZiRFkj

csylksaMkcsylksaM

kegkleqan 2,35,27

61.62 NA 18.10.

18

&&^^&&^^&&

12

71

Jh cynkÅ panzkdj vk0 Jh ukjk;.k panzkdj

xzke cjcliqj rglhy o ftyk

egkleqan

18.6.092607/

30.9.0911.9.09

4.9.09 to

3.9.19

Q'khZiRFkj

cjcliqjcjcliq

jegkleqan 166/1 0.15 NA 2.9.18

&&^^&&^^&&

72

Jh fczts'k panzkdj vk0 Jh

eksgu yky panzkdj

xzke cjcliqj rglhy o ftyk

egkleqan

8.4.091208/ 8.6.09

22.5.0919.5.09

to 18.5.19

Q'khZiRFkj

cjcliqj cjcliqj

egkleqan178/4,180

181/40.33 NA 17.5.1

8

&&^^&&^^&&

73

Jh fd'kksj lpnso vk-Jh eqjyh/kj

lpnso

jkfte rglhy jkfte ftyk jk;iqj

24.1.081176/ 4.6.09

5.6.0926.5.09

to 25.5.19

Q'khZiRFkj

vNksyh vNksyh egkleqan179717981799

0.12 NA 24.5.18

Nfcyky lkgw fuoklh vNksyh ftyk egkleqa

n

&&^^&&^^&&

74

Jherh fp=ys[kk panzkdj ifr Jh fo".kq jke panzkdj

xzke vNksyh rglhy o ftyk

egkleqan

8.6.092659/

7.10.0928.10.09

26.9.09 to

25.9.19

Q'khZiRFkj

vNksyh vNksyh egkleqan 1111 0.2 NA 24.9.18

&&^^&&^^&&

75

Jh >kykjke panzkdj vk0 Jh

,eu yky panzkdj

xzke cjcliqj rglhy o ftyk

egkleqan

6.1.0121389/

21.6.01210.9.12

10.9.12 to

9.9.22

Q'khZiRFkj

cjcliqj cjcliqj

egkleqan168,169,177

0.5 NA 8.9.21&&^^&&^^&&

76

Jh jktsUnz panzkdj vk0 Jh

[kkseu yky panzkdj

egkleqan rglhy o ftyk

egkleqn

2.6.07536/

17.3.0827.3.08

11.12.07 to

10.12.17

pwukiRFkj

cjcliqjcjcliq

jegkleqan 311,

2441.67 NA 9.12.1

6

&&^^&&^^&&

uohuhdj.k

77

Jh jks'ku nsokaxu v0 Jh [ksnjke nsokaxu

fQaxs'oj rg- jkfte

ftyk xfj;kcan

15.2.0111846/

19.9.1123.9.11

23.9.11 to

22.9.21

Q'khZiRFkj

vNksyh vNksyh egkleqan1713,1714,1716,

0.12 NA 21.9.20

&&^^&&^^&&

13

78

[knku dkexkj

lg- lfefr ?kksMkjh

xzke ?kksMkjh rglhy o ftyk

egkleqan

10.7.061861/

22.12.0613.3.07

17.11.07 to

16.11.17

Q'khZiRFkj

?kksMkjh ?kksMkjh egkleqan 223 0.46 NA 15.11.16

&&^^&&^^&&

79

Jh [kkseu yky

panzkdj vk0 Jh

fcgkjhyky panzkdj

xzke fcjdksuh rglhy o ftyk

egkleqan

11.7.082958/

26.10.1027.3.08

11.12.07 to

10.12.17

pwukiRFkj

cjcliqjcjcliq

jegkleqan 208 1.95 NA 20.3.1

8

&&^^&&^^&&

80

Jh /khjt dksgyh vk-Jh ujs'k dksgyh

xzke ?kksMkjh rglhy o ftyk

egkleqan

5.1.0103134/

12.11.103.2.11

20.10.10 to

19.10.20

Q'khZiRFkj

?kksMkjh ?kksMkjh egkleqan 132 0.86 NA 18.10.19

&&^^&&^^&&

81

Jh vuqie vxzoky

iqjkuh cLrh jk;iqj

rglhy o ftyk jk;iqj 16.7.09

2490/9.11.09 19.11.09

6.11.09 to

5.11.19Q'khZiRFkj vNksyh vNksyh egkleqan

1405/21407140414091276 2.00

NA

4.11.18

82

Jherh usgk vxzoky ifr Jh f'kjh"k vxzoky

xzke ?kksMkjh rglhy o ftyk

egkleqan 1.12.06336/

25.2.11 21.3.11

21.3.11 to

20.3.16

Q'khZiRFkj ?kksMkjh ?kksMkjh egkleqan 74/1 0.3

NA19.3.1

5

&&^^&&^^&&

83

Jh Hkkxor gfjr vk-Lo- Jh lq[kyky

fQaxs'oj rg- jkfte

ftyk xfj;kcan 15.12.10

471/ 7.3.11 15.3.11

15.3.11 to

14.3.21Q'khZiRFkj vNksyh vNksyh egkleqan 14 1

NA13.3.2

0

&&^^&&^^&&

84

Jh fMys'oj izlkn <hej vk0 Jh m/kksjke <hej

xzke ukanxkao

rglhy o ftyk

egkleqan 23.4.11694/

31.3.11 24.3.11

24.3.11 to

23.3.21

Q'khZiRFkj ukanxkoa ukanxkao egkleqan

3266,3267,

3271/1,3274/1 0.65

NA22.3.2

0

&&^^&&^^&&

85

Jherh bUnzk.kh ckbZ xqIrk ifr Jh larks"k xqIrk

LVs'ku ikjk egkleqan 23.4.11

1661/ 3.9.11 8.9.11

8.9.11 to

7.9.16Q'khZiRFkj vNksyh vNksyh egkleqan 1776 0.22

NA

6.9.15

&&^^&&^^&&

14

86 Jh lkses'k

nos vk0 Jh th-,l- nos

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rglhy o ftyk

egkleqan 13.8.091677/ 3.9.11 23.9.11

23.9.11 to

22.9.21

Q'khZiRFkj ?kksMkjh ?kksMkjh egkleqan 9,10 0.59

NA

21.9.20

&&^^&&^^&&

87 Jh Hkksykjke

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dkslkuxj usg: uxj iwoZ fHkykbZ ftyk nqxZ 7.2.11

1673/ 3.9.11 27.9.11

27.9.11 to

26.9.16Q'khZiRFkj vNksyh vNksyh egkleqan

1270/2,1271,1272,1273, 0.3

NA

25.9.15

&&^^&&^^&&

88

Jh gsear panzkdj vk-Jh mRre pnzkdj

xzke cjcliqj rglhy o ftyk

egkleqan 16.5.112091/

18.10.011 24.10.11

24.10.11 to

23.10.16

Q'khZiRFkj cjcliqj

cjcliqj egkleqan 178/2 0.18

NA

22.10.15

&&^^&&^^&&

89

Jh bnzlsu HkkaMsdj vk0 Jh uanwjke HkkaMsadj

jkfte rglhy jkfte ftyk jk;iqj 18.10.11

2531/ 27.12.11 10.1.12

10.1.12 to

9.1.17Q'khZiRFkj cjcliqj

cjcliqj egkleqan 187/1 0.3

NA

8.1.16

&&^^&&^^&&

90

Jh ujsUnz lq;Zoa'kh vk-Jh jkeyky lq;Zoa'kh

v;ks/;kuxj egkleqan

31.3.112509/

24.12.1112.1.12

12.1.12 to

11.1.17

Q'khZiRFkj

vNksyh vNksyh egkleqan 1806,1807,

0.3 NA 10.1.16

&&^^&&^^&&

91

Jh lqjs'k panzkdj vk-Jh eksgu panzkdj

iqjkuk jk;iqj ukdk egkleqan ftyk

egkleqan

13.9.11412/

15.2.123.3.12

3.3.12 to

2.3.22

Q'khZiRFkj

cjcliqj cjcliqj

egkleqan 207 0.72 NA 1.3.21&&^^&&^^&&

92

Jh fgjsUnz lkgw

egkleqan rglhy o ftyk

egkleqn

22.6.09430/

15.2.0121.3.12

23.6.10 to

22.6.20

pwukiRFkj cjcliqj

cjcliqj egkleqan 177.

186/20.56 NA 21.6.1

9

>kykjke panazkdj fuoklh cjcliqj rglhy o ftyk egkleqa

&&^^&&^^&&

15

n

93

Jh >kykjke panzkdj vk0 Jh

,eu yky panzkdj

xzke cjcliqj rglhy o ftyk

egkleqan

4.10.07422/

15.2.121.3.12

23.6.10 to

22.6.20

pwukiRFkj

cjcliqjcjcliq

jegkleqan 210 0.41 NA 21.6.1

9

&&^^&&^^&&

94

Jh lquhy vxzoky vk-

Jh jkevokrkj vxzoky

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7.5.121418/

25.6.125.9.12

5.9.12 to

4.9.17

pwukiRFkj

vNksyh vNksyh egkleqan

780/2,781,783,784

0.41 NA 3.9.16&&^^&&^^&&

95

Jh v'kksd flag

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jktiwr

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14.6.122236/

3.11.1215.7.13

15.7.13 to

14.7.23

Q'khZiRFkj

vNksyh vNksyh egkleqan

83,93,94,95,

96,97/2

0.58 NA 13.7.22

&&^^&&^^&&

440/ 5.7.1312000

mt

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Jherh dqys'ojh ckbZ ifr Jh ckyd

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14.6.122234/

3.11.1215.7.13

15.7.13 to

14.7.23

Q'khZiRFkj

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1359,1360,1362,1370,1372,1375,1377,

1379/2,1382,1386,1387,1389,1392

0.49 NA 13.7.22

&&^^&&^^&&

442/ 5.7.1315000

mt

16

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Jh f'ko dq-jk=s vk-Lo- Jh

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egkleqan

8.8.124406/

2.8.01326.8.13

26.8.13 to

25.8.23

Q'khZiRFkj

?kksMkjh ?kksMkjh egkleqan 31 0.8 NA 24.8.22

&&^^&&^^&&

98

Jh lkabZ Hk.Mkj

lapkyd Jh /khjszUnz

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128 Dyc ikjk

rglhy o ftyk

egkleqan

18.12.124782/

19.12.1321.1.14

21.1.14 to

20.1.24

Q'khZiRFkj

cjcliqjcjcliq

jegkleqan 186/1 0.42 NA 19.1.2

3

&&^^&&^^&&

423/ 2.7.013 40000 Cum

99

es-ch-,l-lh-ih-,y- fy-izks- Jh th-,l-ds-jko

xzke ?kksMkjh rglhy o ftyk

egkleqan

20.4.0121040/

30.4.1210.5.12

10.5.12 to

9.5.22

Q'khZiRFkj

cjcliqj cjcliqj

egkleqan 177 1.6 NA 8.5.21&&^^&&^^&&

618/ 6.8.13 120000 Sp

100

Jh jkekuqt panzkdj vk-Jh Vseu yky

panzkdj

xzke cjcliqj rglhy o ftyk

egkleqan

6.8.124852/

27.12.134.1.14

4.1.14 to

3.1.24

Q'khZiRFkj cjcliqj

cjcliqj egkleqan 193,

187/20.65 NA 2.1.23

&&^^&&^^&&

6

Jh lkabZ Q'khZ m?kksx lapkyd Jh vt; flag Bkdqj vk-Lo- Jh nyxtu flag Bkdqj

xzke eq<suk rglhy o ftyk

egkleqan

19.2.13127/

22.1.1428.1.14

23.2.14 to

22.2.24

Q'khZiRFkj

eq<suk eq<suk egkleqan 333/2 0.54 NA 21.2.23

&&^^&&^^&&

1044/ 29.11.013 1000Cum

102

Jh lq'khy tkaxMs vk-Jh jkejru

tkaxMs

xzke ?kksMkjh rglhy o ftyk

egkleqan

31.1.13134/

22.1.1428.1.14

28.1.14 to

27.1.24

Q'khZiRFkj ?kksMkjh ?kksMkjh egkleqan 87,88 0.34 NA 25.1.2

3

&&^^&&^^&&

7

Jh jks'ku vxzoky vk-Jh iou vxzoky

dkyst jksM egkleqan

22.5.091034/

25.5.0925.5.09

22.5.09 to

21.5.19

Q'khZiRFkj

eq<suk eq<suk egkleqan 331,333/1

0.26 NA 20.5.18

&&^^&&^^&&

17

104

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3 Jh xw:eq[k

flag ja/kkok 4 Jh fcjsUnzj

flag phek

egkleqan rglhy o ftyk

egkleqn

12.1.09390/

4.2.0918.2.09

28.1.09 to

27.1.19

feV~Vh ¼fpeuh

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egkleqan 3, 2 1.15 NA 26.1.2018

&&^^&&^^&&

105

Jherh lkfo=h

panzkdj fr Jh lqjsUnz panzkdj

egkleqan rglhy o ftyk

egkleqn

9.4.10592/

22.3.119.5.11

21.3.11 to

20.3.21

feV~Vh ¼fpeuh

½eksj/kk eksj/kk egkleqan 5,2 0.58 NA 19.3.2

0

&&^^&&^^&&

106

es phek fczDl egk-ikVZuj 1 Jh txchj flag phek

2 Jh tliky flag phek

3 Jh xw:eq[k

flag ja/kkok 4 Jh fcjsUnzj

flag phek

egkleqan rglhy o ftyk

egkleqn

19.2.10512/

9.3.1118.4.11

3.3.11 to

2.3.21

feV~Vh ¼fpeuh

½vNjhMhg vNjhMh

gegkleqan 354,

355,0.34 NA 1.3.20

&&^^&&^^&&

107

Jherh yrk panzkdj ifr Jh thojkt panzkdj

xzke yHkjk[kqnZ rg- o ftyk

egkleqan

3.10.07870/

15.5.0827.5.08

27.5.08 to

26.5.18

feV~Vh ¼fpeuh

½

lkYgsHkkBk

lkYgsHkkBk

egkleqan dqy 7 0.89 NA 25.5.18

&&^^&&^^&&

108

Jherh vxs'ojh panzkdj ifr Jh iadt panzkdj

f=ewfrZ dkWyksuh

rglhy o ftyk

egkleqan

7.9.061409/

18.10.0627.11.06

25.11.06 to

24.11.16

feV~Vh ¼fpeuh

½dusdsjk dusdsjk egkleqan dqy 19 2.7 NA 23.11.

15

&&^^&&^^&&

2378/ 12.10.0620.00 Lakh Nose

18

109

Jh fot; xqIrk vk0 Jh frjFk jke xqIrk

LVs'ku ikjk egkleqan 16.1.06

1399/ 11.10.06

2.11.062.11.06

to 1.11.16

feV~Vh ¼fpeuh

½xksikyiqj

xksikyiqj

egkleqan dqy 17 2.63 NA 30.10.06

&&^^&&^^&&

110

Jherh yrk panzkdj ifr Jh thojkt panzkdj

xzke yHkjk[kqnZ rg- o ftyk

egkleqan

24.11.06685/

15.3.0727.3.07

15.3.07 to

14.3.17

feV~Vh ¼fpeuh

½'ksj 'ksj egkleqan dqy 20 2.01 NA 13.3.1

6

&&^^&&^^&&

111

es phek fczDl egk-ikVZuj 1 Jh txchj flag phek

2 Jh tliky flag phek

3 Jh xw:eq[k

flag ja/kkok 4 Jh fcjsUnzj

flag phek

egkleqan rglhy o ftyk egkleqn

28.12.07961/ 9.5.11

27.3.0827.3.08 to 26.3.18

feV~Vh ¼fpeuh½

cMxkao cMxkao egkleqan dqy 5 1.47 NA 25.3.17

&&^^&&^^&&

112

Jherh izhrh 'kekZ ifr Jh lat; 'kekZ

iqjkuh flfoy ykbZu rglhy o ftyk jk;iqj

1.2.11333/ 25.2.11

3.3.1125.2.11 to 24.2.21

feV~Vh ¼fpeuh½

'ksj 'ksj egkleqan dqy 17 2.41 NA 23.2.20

&&^^&&^^&&

3701/ 8.3.1130.00 Lakh

113

Jherh fLerk paanzkdj ifr Jh fgrss'k panzdkj

egkleqan rglhy o ftyk egkleqn

21.2.111063/ 13.5.11

7.7.1112.5.11 to 11.5.21

feV~Vh ¼fpeuh½

/kulqyh /kulqyh egkleqan

1705,1714,1716,1718,1719,1720,

1.6 NA 10.5.20

&&^^&&^^&&

114

Jherh izhrh 'kekZ ifr Jh lat; 'kekZ

iqjkuk flfoy ykbZu rg-o ftyk egkleqan

14.6.112201/ 2.11.11

8.2.12

24.10.11 to 23.10.18

feV~Vh ¼fpeuh½

'ksj 'ksj egkleqan dqy 17 2.48 NA 22.10.17

&&^^&&^^&&

19

115

Jherh 'kkjnk ,ju ifr Jh lqnj ,ju

fu- fiFkkSjk rg-fiFkkSjk ftyk egkleqaan

30.8.06 34/ 3.1.07 16.1.07

26.12.06 to 25.12.16

iRFkj dzs'kj

y{ehiqj y{ehiqj fiFkkSjk 221 1.2 NA 24.12.15

&&^^&&^^&&

116

Jh vkyksd dkuwuxks vk0 Jh r:.k dkuquxks

fuoklh Mxfu;k jk;iqj rglhy o ftyk jk;iqj

19.12.06892/ 10.4.07

20.4.0719.4.07 to 18.4.17

iRFkj dzs'kj

fryatuiqj

lkfo=hiqj

fiFkkSjk 57, 38 0.25 NA 17.4.16

&&^^&&^^&&

861/ 9.4.0723040cum

117

Jh vk'kh"k vxzoky vk-Jh xksfoan vxzoky

fuoklh fiFkkSjk rglhy fiFkkSjk ftyk egkleqan

26.11.076248/ 29.12.07

2.1.08

29.12.07 to 28.12.17

iRFkj dzs'kj

fd'kuiqjfd'kuiqj

fiFkkSjk 569 1.12 NA 27.12.16

&&^^&&^^&&

118

Jh dqyoar flag [kuwtk vk-Jh vthr flag [kutk

okMZ ua- 15 fiFkkSjk rglhy fiFkkSjk ftyk egkleqan

27.5.011693/13.3.12

11.9.1211.9.12 to 10.9.22

iRFkj dzs'kj jkeiqj

fd'kuiqj fiFkkSjk 291 0.92 NA 9.9.20

21

&&^^&&^^&&

119

Jh Vhdepan uk;d vk0Jh lqcus'oj uk;d

xzke dstqaok rglhy ljk;ikyh ftyk egkleqan

29.10.07494/ 5.3.08

14.3.083.3.08 to 2.3.18

iRFkj dzs'kj

HkkywdksukjktkMhg

ljk;ikyh 166 0.32 NA 1.3.17&&^^&&^^&&

570/29.2.085000Cum

120

Jherh ehjk vxzoky ifr Jh fxj/kkjh yky

fu-ljk;ikyh rglhy ljk;ikyh ftyk egkleqan

28.1.08383/ 20.2.08

29.2.0820.2.08 to 19.2.18

iRFkj dzs'kj

pVVhfxjkSyk

pV~VhfxjkSyk ljk;ikyh 45,55 2.78 NA 18.2.1

7

&&^^&&^^&&

20

121

Jh izgykn jk; vxzoky vk-Jh euksgj yky

esu jksM ljk;ikyh rglhy ljk;ikyh ftyk egkleqan

4.8.08233/ 20.1.09

21.1.0915.1.09 to 14.1.19

iRFkj dzs'kj

jktkMhgjktkMhg

ljk;ikyh 103, 104

2.5 NA 13.1.18

&&^^&&^^&&

122

es-ch-,l-lh-ih-,y- fy-izks- Jh th-,l-ds-jko

gky eqdke ?kksMkjh rglhy o ftyk egkleqqn

10.1.121048/ 30.4.12

6.6.1215.5.12 to 14.6.22

iRFkj dzs'kj

NqbZikyh NqbZikyh ljk;ikyh

235, 364, 270, 271, 272, 273,

228/5, 228/6

2.59 NA 13.6.21

&&^^&&^^&&

123

es-ch-,l-lh-ih-,y- fy-izks- Jh th-,l-ds-jko

gky eqdke ?kksMkjh rglhy o ftyk egkleqqn

28.8.142778/ 30.12.14

26.2.1526.2.15 to 25.2.25

iRFkj dzs'kj

fNjkZysokfNjkZysok

cluk 97 3.2 NA 24.2.24

Jh bejku nYyk vk-Lo-Jh bfy;kl nYyk fuoklh ljk;ikyh ftyk egkleqan

&&^^&&^^&&

436 date 7/8/14300 Tane per year

124

Jh lquhy vxzoky vk-Jh jkevokrkj vxzoky

cluk rg-cluk ftyk egkleqan

22.12.092654/ 6.10.10

18.11.1021.1.11 to 20.1.21

iRFkj dzs'kj

/kkeu?kqVdqjh pan[kqjh cluk 343 1.2 NA 19.1.2

0

&&^^&&^^&&

125

Jh fot; vxzoky vk0 Jh jkevorkj vxzoky

cluk rg-cluk ftyk egkleqan

8.3.103626/ 4.1.11

3.2.1118.4.11 to 17.4.21

iRFkj dzs'kj

/kkeu?kqVdqjh

pan[kqjh cluk 343 1.44 NA 16.4.20

&&^^&&^^&&

21

126

Jh fot; vxzoky vk0 Jh jkevorkj vxzoky

cluk rg-cluk ftyk egkleqan

3.9.124807/ 24.12.13

3.1.143.1.14 to 2.1.24

iRFkj dzs'kj

feykjkckn

ukudlkxj

cluk 389 2.86 NA 1.1.23&&^^&&^^&&

966/ 28.11.1330000 Tan

127

Jh lquhy vxzoky vk-Jh jkevokrkj vxzoky

cluk rg-cluk ftyk egkleqan

10.7.124807/ 19.12.13

26.12.13

26.12.13 to 25.12.23

iRFkj dzs'kj

feykjkckn

ukudlkxj

cluk 389 2.58 NA 24.12.24

&&^^&&^^&&

1250/ 12.12.13120000Tan

128

Jh eksfur vxzoky vk0 Jh rqylhnkl vxzoky

cluk rg-cluk ftyk egkleqan

7.11.06689/ 15.3.07

16.4.0715.3.07 to 14.3.17

iRFkj dzs'kj

feykjkckn

ukudlkxj

cluk 370,371

0.72 NA 13.3.16

&&^^&&^^&&

979/ 29.7.1118000 mt

129

es- jruk [kfut v|ksx kzks-Jh lquhy vxzoky vk-Jh jkevorkj vxzoky

cluk rg-cluk ftyk egkleqan

19.1.072807/ 7.8.07

3.9.0724.7.07 to 23.7.17

iRFkj dzs'kj rjsdsy rjsdsyk cluk 618 2.09 NA 22.7.1

6

&&^^&&^^&&

130

Jh jktsUnz 'kekZ vk0 Jh /keZohj 'kekZ

ljk;ikyh rg- o ftyk egkleqan

1.8.073706/ 17.10.07

4.1.08

17.10.07 to 16.10.17

iRFkj dzs'kj

cEguhMhg

[kksxlk cluk 545 0.16 NA 15.10.15

&&^^&&^^&&

1583/ 27.9.075000 Cum

131

Jh Nfcyky iVsy vk0 Jh :i/kj iVsy

lkxjikyh rg- cluk ftykegkleqan

16.5.072794/ 4.8.07

3.9.07

01.08.07 to 31.07.17

iRFkj dzs'kj

culwyhMhg

lkxjikyh

cluk 38,37/1

0.18 NA 29.7.16

&&^^&&^^&&

1774/2.7.7

18000Mt

132

vjfoan ds'kj lapkyd Jh yfyr tSu vk0 Jh cPNjkt tSu

ljk;ikyh rg- o ftyk egkleqan

13.10.082652/ 28.11.08

29.11.08

12.10.08 to 11.10.18

iRFkj dzs'kj yfyriqj cuMcjh cluk 8 0.86 NA 10.10.

17

&&^^&&^^&&

22

133

Jh ftrsUnz d';Ik vk0 Jh ,l- ih-d';I

es-v[kjkHkkBk LVksu ekbZu okMZZ u- 22 QkjsLV vkfQl ds ikl esu jksM rg-cluk ftyk egkleqan

27.12.124780/ 19.12.13

26.12.13

26.12.13 to 25.12.23

iRFkj dzs'kj

v[kjkHkkBk

ukudlkxj cluk

117,322,323,

3.55 NA 24.12.22

&&^^&&^^&&

1012/ 29.11.01363000 Tan

134

Jh t;ar pkS/kjh vk0 Jh 'kkSdhyky pkS/kjh

ijlnk rg-ljk;ikyh ftyk egkleqan

13.2.073869/ 3.11.07

3.1.08

29.10.07 to 28.10.17

iRFkj dzs'kj

Likikyh :ikikyh

cluk 111,112,

2.14 NA 27.10.17

&&^^&&^^&&

2288/ 17.9.0745000Mt

135

wes- mMhlk dkadzhV ,aM ,ykbZM baaMlVªht fy-

Hkuiqjh ftyk jk;iqj

5.8.04947/ 19.7.06

2.11.062.11.06 to 1.11.16

iRFkj dzs'kj

irsjkikyh

irssjkikyh ckxckgjk 28 1.3 NA 31.10.

15

&&^^&&^^&&

136

Jh cyohj flag cSl vk0 Jh tujSy flag

[kfj;kj jksM mMhlk rg-o ftyk uqvkikjk

23.3.05947/ 19.7.06

2.8.0619.7.06 to 18.7.16

iRFkj dzs'kj

irsjkikyh

irssjkikyh

ckxckgjk 28 1.3 NA 17.7.15

&&^^&&^^&&

2011/2.9.510000Cum

137

wes- mMhlk dkadzhV ,aM ,ykbZM baaMlVªht fy-

ckxckgjk ftyk egkleqan

5.8.04396/ 2.3.06

12.7.0612.7.06 to 11.7.16

iRFkj dzs'kj

irsjkikyh

irssjkikyh

ckxckgjk 28 3.5 NA 10.7.15

&&^^&&^^&&

138

Jh nkuohj 'kekZ vk0 Jh fcgkjhyky 'kekZ

ckxckgjk ftyk egkleqan

30.6.062289/ 31.5.07

11.6.0722.7.07 to 21.7.17

iRFkj dzs'kj

fcjktikyh

fcjktikyh

ckxckgjk 85 3.6 NA 20.7.16

&&^^&&^^&&

139

Jh vCnqy jghe [kku vk0 Jh vCnqy erhu [kku

okMZ u- 13 [kfj;kj jksM+ mMhlk

3.12.081090/ 27.5.09

27.5.0920.5.09 to 19.5.19

iRFkj dzs'kj

iVijikyh [kqnZ

iVijikyh [kqnZ

ckxckgjk 11 1.25 NA 18.5.18

Jh d`".k dqekj vxzoky fuoklh ckxckgjk

&&^^&&^^&&

23

ftyk egkleqan

140

Jh eqds'k lkgw vk0 Jh <kyw jke lkgw

xkatj rg-ckxckgjk ftyk egkleqan

29.6.092365/ 11.8.09

5.9.094.3.09 to 3.3.19

iRFkj dzs'kj

NbZgk NqbZgk ckxckgjk 1206 1 NA 2.3.18&&^^&&^^&&

141

Jherh va'kq vxzoky ifr Jh lat; vxzoky

ckxckgjk ftyk egkleqan

30.6.091379/ 10.5.10

5.7.1028.4.10 to 27.4.20

iRFkj dzs'kj

dkslejkZ dkslejkZ ckxckgjk 284 1.15 NA 26.4.19

Jh ujs'k vxzoky fuoklh [kfj;kj jksM mMhlk

&&^^&&^^&&

589/ 20.3.061000 Cum

142

Jh fgrs'k panzdkj vk0 jh uk;d jke panzkdj

egkleqan rglhy o ftyk egkleqn

22.11.061845/ 21.12.06

23.12.06

20.12.06 to 19.12.16

iRFkj dzs'kj

rsyhcka/kk rsyhcka/kk

ckxckgjk 107 0.82 NA 18.12.15

&&^^&&^^&&

1466/ 4.12.06200000 cft

143

Jh iou dqekj panzkdj vk0 Jh eugj.k yk pnzkdj

gkMkcan rg-ckxckgjk o ftyk egkleqan

28.3.061416/ 18.10.06

8.11.068.11.06 to 7.11.16

feV~Vh ¼fpeuh½

Mksxjhikyh

Mksxjhikyh

ckxckgjk 14 1.01 NA 6.11.15

&&^^&&^^&&

144

es- mMhlk dzkadzhV ,yk- baM-fy-lpkyd Jherh laxhrk vxzoky ifr Jh izeksn vxzoky

jk;iqj rg-o ftyk jk;iqj

23.5.12 30/ 4.1.14 21.1.1421.1.14 to 20.1.24

xzukbZV ¼;af=d fdz;k }kjk fxVVh cukus gsrq½

gkMkcan gkMkcan ckxckgjk 518 1.27 NA 19.1.23

&&^^&&^^&&

1077/ 24.3.0960000mt

24

145

es- mMhlk dzkadzhV ,yk- baM-fy-lpkyd Jh peqHkZt vxzsoky

jk;iqj rg-o ftyk jk;iqj

23.5.12 30/ 4.1.14 21.1.1421.1.14 to 20.1.24

xzukbZV ¼;af=d fdz;k }kjk fxVVh cukus gsrq½

gkMkcan gkMkcan ckxckgjk 518 1.4 NA 19.1.23

&&^^&&^^&&

146

Jh iadt vxzoky vk-Jh cztjkt vxzoky

iqjkuh xate.Mh ds ikl lqHkk"k jksM jk;iqj

31.194

3-82/95/12/1date 27.8.96

25.3.97

25.3.97 to 24.3.17

DokVZt mMsyk mMsyk ljk;ikyh '19/1 2.21 NA23.3.16

IBM/10668/2012

147

Jherh xkserh iVsy ifr Lo-Jh lq[kyky iVsy

xzke cVdh rg-ljk;ikyh ftyk egkleqan

23.3.12

3-169/97/12/1Date 22.8.98

23.3.99

23.3.99 to 22.3.19

Qk;jDys cujMhg cujMhg ljk;ikyh

14/114/2 0.769 NA

21.3.18

&&^^&&^^&&

IBM/9872/2012

148

Jh fnus'k 'kekZ vk-Jh iwju pan 'kekZ

gky eqdke jk;iqj rg0 o ftyk jk;iqj

17.11.04

f-3-3/5/12 Date 12.7.05

6.5.04

27.7.05 to 26.7.25

DokVZt[kq'khZigkj

[kq'khZigkj fiFkkSjk

564566 1.51 NA

25.7.24

&&^^&&^^&&

IBM/9572/2012

149

Jh fnus'k 'kekZ vk-Jh iwju pan 'kekZ

gky eqdke jk;iqj rg0 o ftyk jk;iqj

9.2.15

f-3-20/5/12 Date 12.7.05

23.9.06

15.9.06 to 14.9.26

DokVZtlkYgsrjkbZ

lkYgsrjkbZ fiFkkSjk 639 1.6 NA

13.9.25

&&^^&&^^&&

IBM/9572/2012

150

Jh jkts'k 'kekZ vk-Jh iwjupan

gky eqdke jk;iqj rg0 o ftyk jk;iqj

8.4.05

f-3-48/05/12 Date21.12.06

27.12.06

2.1.07 to 1.1.27

DokVZt

dksfy;kjh Mhg

dksfy;kjh Mhg

cluk 694 2.4 NA30.12.25

&&^^&&^^&&

IBM/10484/2012

151

Jh yfyr vxzoky vk-Jh jktsUnz vxzoky

ckxckgjk ftyk egkleqan

1.2.07

f-2-33/5/12 Date 4.7.06

6.10.08

6.10.08 to 5.10.18

DokVZt

iVijikyh [kqnZ

iVijikyh [kqnZ

ckxckgjk 639 1.48 NA 4.1.17

&&^^&&^^&&

IBM/10626/2012

152

Jh jfo tSuvk-Jh uhyepan tSu

fu-egkleqan rglhy o ftyk egkleqan 9.10.09

f-2-25/10812 Date 8-11-10

21.9.11

19.9.11 to 18.9.31

DokVZt fNankSyh fNankSyh egkleqan 181 4.2 NA17.9.30

&&^^&&^^&&

IBM/10626/2012

25

153

Jh [kseyky panzkdj

xzke fcjdksuh rglhy o ftyk

egkleqan

20.12.13463/21.2.14

6.3.14

6.3.14 to 5.3.24

Q'khZiRFkj cjcliqj Cjcliqj egkleqan 467 0.5 NA 5.3.23

Ik;kZoj.k vukifRr izek.k i= izkIr

154

Jh jkekuqt panzkdj vk-Jh Vseu yky panzkdj

xzke cjcliqj rglhy o ftyk egkleqan

13.7.111799/

13.9.11 28.9.11

28.9.11 to 27.9.21

pwukiRFkj cjcliqj Cjcliqj egkleqan 212 0.75 NA

26.9.20

&&^^&&^^&&

155

>kykjke panzkdj vk-Jh ,eu yky panzkdj

xzke cjcliqj rglhy o ftyk egkleqan

4.10.07

2907/16.12.07

4.10.08 to 3.10.18

pwukiRFkj cjcliqj Cjcliqj egkleqan 311 0.4 NA

2.10.17

&&^^&&^^&&

156

>kykjke panzkdj vk-Jh ,eu yky panzkdj

xzke cjcliqj rglhy o ftyk egkleqan

22.609

422/15.2.12

1.3.12

23.6.10 to 22.6.20

pwukiRFkj cjcliqj Cjcliqj egkleqan 210 0.41 NA

21.6.19

&&^^&&^^&&

157

Jh fVds'oj iVsy ikVZuj Jh dUgS;k yky vxzoky

xzke eks[kkiqVdk rglhy cluk ftyk egkleqan

11.10.10

f-3-51/2010/12 date 31-10-14

20.4.15

20.4.15 to 19.4.35

DokVZt [kksxlk [kksxlk cluk

311/1313455/2455/1456 4.08 NA

18.4.34

&&^^&&^^&&

158

Jh lakbZ HkaMkj lpkyd Jh /khjsUnz yks.kkjs vk-Jh uhydekj yks.kkjs fuoklh 128 Dyc ikjk egkleqan

xzke cjcliqj rglhy o ftyk egkleqan

18.12.15

4782/ 19.12-13

21.1.16

21.1.14 to 20.1.24

Q'khZiRFkj cjcliqj

Ckjcliqj egkleqan 186/1 0.42 NA

19.1.23

&&^^&&^^&&

617/5.5.13

4. Details of Royalty or Revenue Received in Last Three Year

(i) Major Minerals

In Mahasamund district there have no any mining lease.

(ii) Details of Royalty or Revenue Received in Last Three Year

Minor Minerals

S.No.

Mineral Royalty or Revenue Received2013-14 2014-15 2015-16

Production Royalty(Rs.)

Production(Tonne)

Royalty(Rs.)

Production(Tonne)

Royalty(Rs.)

1 Quartz 11098 tonne 832365 16493 tonne 1237000 34313 tonne 25735002 Stone Bolder 1070 m3 110210 790 m3 81370 - -3 Stone Crusher 69315m3 7139456 269206 m3 27728179 50411 m3 5192300 m3

4 Limestone 3634 tonne 228939 2767 tonne 174328 7132 tonne 570575 tonne5 Flagstone

(farsi stone)163931 m3 16884878 183266 m3 18876381 256305 m3 26399422 m3

6 Soil(Chimney) 71605 m3 1432100 52200 m3 1044000 81875 m3 16375007 Lateritic soil

(murram)241000 m3 4820000 307550 m3 6151000 256300 m3 5126000

m3

Total 3144794 55292258 41499297

1

5.Details of Production & Royalty of Sand in last Three yearsOrdanary Sand

S.No. Financial Year Production of Sand (in M3) Royalty Recieved in Rs.

1 2013-14 260989.5 5219490

2 2014-15 130006 2600120

3 2015-16 2774600 2774600

ftyk jktukanxkao esa fnukad 15-05-2016 dh fLFkfr esa ?kksf"kr jsr ?kkVks dh tkudkjh

S.no. Mine(Village) name

Khasara no. Area Duration

1 Barbaspur (a) 1 4.00 Hect. 21.11.2013 to 20.11.20162 Barbaspur (b) 175 4.00 Hect. 21.11.2013 to 20.11.20163 Ghodari 1 4.00 Hect. 21.11.2013 to 20.11.20164 Achholi 1 4.00 Hect. 23.12.1013 to 22.12.20165 Mohakam 1 14.00 Hect. 06.11.2015 to 05.11.20176 Khadsa 1 15.00 Hect 06.11.2015 to 05.11.20177 Kanekera 2604 7.00 Hect. 08.02.2016 to 07.02.20188 Navgaon 3151,3152 15.00 Hect. 15.03.2016 to 14.03 2018

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6. PROCESS OF DEPOSITION OF SEDIMENTS IN THE RIVERS

The district forms a part of the Mahanadi basin. The general slope on the eastern part of the area is towards south –east, in the central part of the area is towards north and on the western part is towards north western direction. The western boundary of the district is running along the Mahanadi River . The Jonk River passes through the central part of the district and is running in northern direction. The Kurar nala, Nami nala, Keswa nala and sukha nadi forms part of the drainage system for Mahanadi River basin. the Mechka nala, Bagh nala, Racme nala Lath nala forms part of the Jonk River basin. The Kunti nala, Surangi nala and Chinar nala forms part of the Ong River basin.

The obvious things rivers transportload, erode load and erode the channel through which they flow. Erosion Erosion is the breaking down of material by an agent. In the case of a river, the agent is water. The water can erode the river’s channel and the river’s load. A river’s load is bits of eroded material, generally rocks, which the river transports until it deposits its load. A river’s channel is eroded laterally and vertically making the channel wider and deeper. The intensity of lateral and vertical erosion is dictated by the stage in the river’s course, discussed in more detail here but essentially, in the upper stage of the river’s course (close to the source of the river) there is little horizontal erosion and lots of vertical erosion. In the middle and lower stages vertical erosion is reduced and more horizontal erosion takes place.

There are several different ways that a river erodes its bed and banks. The first is hydraulic action, where the force of the water removes rock particles from the bed and banks. This type of erosion is strongest at rapids and waterfalls where the water has a high velocity. The next type of erosion is corrasion. This is where the river’s load acts almost like sandpaper, removing pieces of rock as the load rubs against the bed & banks. This sort of erosion is strongest when the river is transporting large chunks of rock or after heavy rainfall when the river’s flow is turbulent.

Corrosion is a special type of erosion that only affects certain types of rocks. Water, being ever so slightly acidic, will react with certain rocks and dissolve them. Corrosion is highly effective if the rock type of the channel is chalk or limestone (anything containing calcium carbonate) otherwise, it doesn’t have much

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of an effect. Cavitation is an interesting method of erosion. Air bubbles trapped in the water get compressed into small spaces like cracks in the river’s banks. These bubbles eventually implode creating a small shockwave that weakens the rocks. The shockwaves are very weak but over time the rock will be weakened to the point at which it falls apart. The final type of erosion is attrition. Attrition is a way of eroding the river’s load, not the bed and banks. Attrition is where pieces of rock in the river’s load knock together, breaking chunks of rock off of one another and gradually rounding and shrinking the load.

Transportation When a river erodes the eroded material becomes the river’s load and the river will then transport this load through its course until it deposits the load. There are a few different ways that a river will transport load depending on how much energy the river has and how big the load is. The largest of particles such as boulders are transported by traction. These particles are rolled along the bed of the river, eroding the bed and the particles in the process, because the riverdoesn’t have enough energy to move these large particles in any other way. Slightly smaller particles, such as pebbles and gravel, are transported by saltation. This is where the load bounces along the bed of the river because the river has enough energy to lift the particles off the bed but the particles are too heavy to travel by suspension. Fine particles like clay and silt are transported in suspension; they are suspended in the water. Most of a river’s load is transported by suspension. Solution is a special method of transportation. This is where particles are dissolved into the water so only rocks that are soluble, such as limestone or chalk, can be transported in solution. Capacity & Competence Rivers can only carry so much load depending on their energy. The maximum volume of load that a river can carry at a specific point in its course is called the river’s capacity. The biggest sized particle that a river could carry at a specific point is called the river’s competence.

Deposition To transport load a river needs to have energy so when a river loses energy it is forced to deposit its load. There’s several reasons why a river could lose energy. If the river’s discharge is reduced then the river will lose energy because it isn’t flowing as quickly anymore. This could happen because of a lack of precipitation or an increase in evaporation. Increased human use (abstraction) of a river could also reduce its discharge forcing it deposit its load. If the gradient of the river’s course flattens out, the river will deposit its load because it will be travelling a lot slower. When a river meets the sea a river will deposit its load because the gradient is generally reduced at sea level and the sea will absorb a lotof

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energy. As rivers get nearer to their mouths they flow in increasingly wide, gentle sided valleys. The channel increases in size to hold the extra water which the river has to receive from its tributaries. As the river gets bigger it can carry larger amounts of material.

This material will be small in size, as larger rocks will have broken up on their way from the mountains. Much of the material will be carried in suspension and will erode the river banks by abrasion. When rivers flow over flatter land, they develop large bends called meanders. As a river goes around a bend most of the water is pushed towards the outside causing increased erosion.

The river is now eroding sideways into its banks rather than downwards into its bed, a process called lateral erosion. On the inside of the bend, in contrast, there is much less water. The river will therefore be shallow and slow-flowing. It cannot carry as much material and so sand and shingle will be deposited. This is called a point bar or slip off slope Due to erosion on the outside of a bend and deposition on the inside, the shape of a meander will change over a period of time. Notice how erosion narrows the neck of the land within the meander. In time, and usually during a flood, the river will cut right through the neck. The river will then take the new, shorter route.

The fastest current, called the thalweg, will now tend to be in the centre of the river, and so deposition is likely to occur in gentler water next to the banks. Eventually deposition will block off the old meander to leave an oxbow lake. The oxbow lake will slowly dry up , only refilling after heavy rain or during a flood. Streams lose velocity and make deposits when their gradient decreases, when the vwater decreases, when there is an increase in cross section, when they encounter obstructions, or when they enter still water. They deposit alluvial fans, alluvial cones, piedmont alluvial plains, channel fill, bars, flood plains and deltas.

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7. General Profile of the District

S.No. Particulars Statistics1 General Information

Geographical Area 4790 sq. kmGeographical Position 20º49’30” to21º33’07”

81º59’56” to 83º16’10”Administrative Division/Number of Tehsil 5No. of Panchayat/Villages 1145Population (As Per Census 2011) 1032275Population Density (As Per Census 2011) 260/km2 (690/sq mi)

2 GeographologyMajor Physiographic Units Granite, Limestone, Flag

Stone, Gold and Tin,Lead ore, Fluorite,Beryl etc.

Major Drainage Mahanadi River, sukha nala, Nami nala, Machka nala, Jonk nala, Racmel nala, Lillar nala,nLath nala and Surangi nala.

3 Land use (Km2)Forest Area 98610.145 Hact.

4 Major Soil Types5 Number of Ground Water Monitoring Stations of CGWB (10.05.2016)

Water Level 27 mtr.No. of Stop Dam 03No. of Anikat 14No. of Major Bridges

6 HydrologeologyMajor Water Bearing FormationPre-Monsoon depth of water level During 2012Post Monsoon depth of water level during 2012

7 Mining ScenarioTotal No. of Mining Leases (Major Minerals NilTotal Area of Mining Leases (Major Minerals) NilTotal Royalty or Revenue Received from Major Minerals in 2015-16

.

Total No. of Mining Leases (Minor Minerals) 158Total No. of Mining Leases (Minor Minerals)Total Royalty or Revenue Received from Minor Minerals in 2015-16

6,86,79,281

Total No. Notified Sand Leas 08Total Area of Sand Leases 67 Hect.

Total Production of Sand in 2015-16 2774600No. of Quarry lease extended As per Amended CGMMR 2015

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8. Land Utilition Pattern in the Horticulture, Mining etc

i. Horticulture:

ii.Forest :

Land Utilition Pattern in the district: Forest, Agriculture, Horticulture, Mining etc.

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Forest, Agriculture,

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ii)Agriculture and Irrigation:

Chhattisgarh State is known as Rice Bowl of central India about 80% of the population in the state is engaged in agriculture. Mahasamund district is one of the richest bio-diversity area in the state. To reduce the farmersdependence

on rainfall, Government is working towards increasing the irrigation potentiaof the district.on rainfall, Government is working towards increasing the irrigation potentia

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on rainfall, Government is working towards increasing the irrigation potential

iii. River :

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iv)Transportation :

Mahasamund district has three National Highway which are National Highway 6,National Highway 217 and National Highway 216. The construction of four lane road in National Highway 6 from Arang-Mahasamund to Saraipali up to Orisa is in progress. Mahasamund station is well connected to Raipur, Durg, Nagpur, Mumbai, Delhi, Bhopal, sambalpur, Ttilagarh, Vishakhapatnam, Tirupati, Puri, Bilaspur, Koraba, Jodhpur, Ajmer, Ahemdabad etc. through the Indian railway system.

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9. Physiography of the District

Physiographically, the major area of the Mahasamund district exhibits pediment/ pediplain landforms. The other landforms are structural plain, structural hills and velleys, dedudational slope, denudetional hills and velleys in the western and eastern part and floodplain including in filled river beds along the course of Mahanadi River. The district forms a part of Mahanadi basin. the general slope of eastern, central and western parts of the district is towards southeast, north and northwest direction respectively. The tributaries of Mahanadi River drain the district.

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10. Rainfall of District Rajnandgaon Month wise

ftys esa eklokj o’kkZ dh tkudkjh fuEukuqlkj gS %

11. Geology and Mineral

1. Geology :-

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1.1 .Archaean :-

Rock formations ranging in age from Archean to Neo Proterozoic are exposed in the district. The flood plains of Mahanadi River are occupied by recent alluvium. The oldest rocks in the area arerepresented by Bengpal Group of Archean age (>2500 m.y.) and are exposed in the cetral part of the district Bengpal Group comprises grey granite gneiss. Porphyroblastic gneiss and magmatite with enclaves of quartzite, banded amphibole-magnetite quartzite, fuchsite quartzite ,quartz-mica schist, andalucite schist, meta-ultramafic. The rocks of the Sonakhan Group of Paleao Proterozoic age (2200-2000m.y.) comprising meta volcanic and associated meta-sedimentaries, unconformably overlie the gneissic complex and exposed in the northeastern part of the district.

Sonakhan Group is classified into three formations viz. Baghmara, Arjuni and Bilari. Baghmara formation comprises meta-ultramafic amphibolite, actinolite-chlorite schist and basaltic agglomerate. Arjuni Formation comprises meta-conglomerate,meta-greywacke, meta- argillite with banded ferruginous chert, meta rhyolite, tuff and meta-besalt. Billari formation comprises meta-conglomerate,meta greywacke, meta-argilite, meta-basalt with basaltic conglomerate and agglomerate, meta-rhyolite with agglomerate and tuff, meta-greywacke and dacit. The volcano sedimentary sequence of the Sonakhan Group is intruded by a large gabbroic complex of variable composition like peridolite, pyroxenite,anorthositic gabbro and gabbro.

1.2. PalaeoProterozoic :-

Bundeli/Dongargarh Granitoids of Palaeo Proterozoic age occupy major part of the district. It comprises granodiorite, biotite and hornblende granite, lecogranite and granophyres. Granophyre with well developed micrographic texure is marked as a separate lithounit within the granitoids and is exposed in the southwestern and central part of the district. Numbers of younger intrusive of Meso Proterozoic age (2000-1600 m.y.) viz. gabbro and doleritic dykes and qurtz veins have traversed the granitoids and Sonakhan volcano-sedimentary sequence.

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1.3.Meso to Neo Proterozoic :-

Unformed and unmetamorphosed sedimentary cover sequence of rocks belonging to Chhattisgarh Supergroup of Meso to Neo Proterozoic age (2000-900 m.y.) overlie the granitoids and rocks of Sonakhan Group. The Chhattisgarh Supergroup occupies the eastern and western part of district and is represented by Singhora, Chandrapur and Raipur Group.

Singhora Group of sediments are identified as four litho facies and exposed in the eastern part of district.these four litho facies have been given status of Rehatikhol, Saraipali, Bhalukona and Chhuipali formations arranged in ascending order. Rehatikhol formation is predominantly arenitic facies, resting unconformably over the granitic basement and comprises arkose and feldspathic sandstone with minor intercalations of siltstone and shale with a pebble horizon towards the base. Saraipali formation is the argillite facies and a charecterised dominantly by purple and green shale, banded chert and minor limestone. Bhalukona formation is predominantly arenitic facies and comprises quartz arenite,shale and siltstone. Chhuipali formation is the calc-argillite facies and comprises dominantly variegated shale, ferruginous arenite, chirt and bedded stromatolitic and dolomitic limestone.

Chandrapur Group has been classified into three formationsviz. Lohardih, Chapordih and Kansapathai. Lohardih Formation is mostly arenitic in nature and comprises feldspathic sandstone and ferruginous arenite, wacke arenit, arkos, sub- arkose and chirt with polymictic conglomerate at the base.Chapordih formation is predominatly an argillite facies and comprises black,pink and light grey shale intercalated with arenite bands. Black shale is generally laminated with alternate fine silt-rich lamellae. In the western part of the district, it become arenitiv in nature and comprises sub-arkosic arenite to fine grained arenite intercalated with shale, siltstone and mudstone.kansapather formation is dominantly an arenitic facies and comprises highly matured glouconitic quartz arenite. Charmuria formation of Raipur Group is dominantly a carbonate facies and it is represented by cherty limestone, dark grey bedded pyritiferous and argillaceous limestone and purple phasphatic limestone.

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Minerals :-

In Mahasamund district there are no economic minerals deposits of any significance except reported occurrence of fluorite and molybdenum. Fluorite occurring as veins and veinlets in sheared feldspathic quartzite is reported at Charkuta, Chiwrakuta, Chatkachar and Makannuta. Molybdenum occurring in the form of specks in pink granite and granodiorite is reported at 10 km southwest of Sankra.

Other Drainage syste

Sand is mined from the bank of Shivnath, Patesri, Kotri, ,Darekasa and,Amner, Surhi and Folk river. Motinala and Tehri Nala also contribute to the sand minning from theminning is granted to Panchyat

¼i½ egRoiw.kZ ufn;ksa vk

eq[; ufn;ksa ds fooj.k lfgr fudklh iz.kkyh %

Other Information of the DistrictDrainage system with description of main rivers

Sand is mined from the bank of Shivnath, Patesri, Kotri, ,Darekasa and,Amner, Surhi and Folk river. Motinala and Tehri Nala also contribute to the sand minning from the respective area along their bank.The lease for sand minning is granted to Panchyat and Janpad.

egRoiw.kZ ufn;ksa vkSj /kkjkvksa dh eq[;&eq[; tkudkjh

eq[; ufn;ksa ds fooj.k lfgr fudklh iz.kkyh %

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Sand is mined from the bank of Shivnath, Patesri, Kotri, ,Darekasa and,Amner, Surhi and Folk river. Motinala and Tehri Nala also contribute to

along their bank.The lease for sand

Sj /kkjkvksa dh eq[;&eq[; tkudkjh

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fuek.kkZ/khu ;kstuk %

1 Lkakdjk ,uhdV

2 eapdkukyk ¼Hkqjdksuh

3 cMs+ lktkikyh ,uhdV

Lkakdjk FiFkkSjk

eapdkukyk ¼Hkqjdksuh½ ,uhdV Hkqjdksuh FiFkkSjk

lktkikyh ,uhdV cMs lktkikyh Cluk

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iFkkSjk

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