## Records of the Geological Survey of India, Volume 120, Parts 2-81867- includes the "Annual report of the Geological survey of India". |

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Page 32

Since the striation lineation is parallel to L , it is obvious that the movement

related to shearing took place parallel to the F , fold axis representing the

represents a ...

Since the striation lineation is parallel to L , it is obvious that the movement

related to shearing took place parallel to the F , fold axis representing the

**direction**of the maximum elongation of the rocks . Thus the shear zone not onlyrepresents a ...

Page 62

pdx.dz and the attraction at P ( x , 0 ) due to the line element in the

: 2a 0 P ( X ' , o ) Х X b 2Gp.z. dx · dz z + ( x - x ) where G is a universal

gravitational constant . Q ( x , z ) Therefore , the gravity effect at P due to

twodimensional ...

pdx.dz and the attraction at P ( x , 0 ) due to the line element in the

**direction**of z is: 2a 0 P ( X ' , o ) Х X b 2Gp.z. dx · dz z + ( x - x ) where G is a universal

gravitational constant . Q ( x , z ) Therefore , the gravity effect at P due to

twodimensional ...

Page 107

In a three - dimensional case of regionalised variables , where samples are

irregularly located and variations in different

the transformed variogram function has been defined as The parameters of the ...

In a three - dimensional case of regionalised variables , where samples are

irregularly located and variations in different

**directions**are not necessarily equal ,the transformed variogram function has been defined as The parameters of the ...

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### Contents

On the occurrence of Thalassinoides burrows from Lameta | 1 |

Stratigraphy and structure of Delhi Supergroup of rocks | 12 |

Structures in Singhbhum shear zone at and around | 27 |

Copyright | |

7 other sections not shown

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### Common terms and phrases

anhydrite associated average axial planes bands Barotiya base basin beds belt Bhim Group block bodies boreholes burrows central channel chert Chitradurga clay deformation Delhi Delhi Supergroup delta deposit depth detailed developed Devgarh direction district drilling east eastern effect environment estimate evaporites exploration field folds formation Geol Geological geometry gold grade granite gravity ground halite Haryana hinge India indicate inlier iron Krishna laterite limb lineation major mineral mineralisation mining minor Nagaur nature observed occur origin parallel pattern phase of folding plain plunge pre-Delhi present quartz Rajasthan range Reef regional represents reserve resulted rocks samples sand scale schist sediments seismic refraction Sendra Group sequence shear shear zone stage strike structures sulphide surface Surv surveys Table tectonic thickness tion trend unit values volcanics western zone