Records of the Geological Survey of India, Volume 120, Parts 2-8Vols. 1- include Report of the Geological Survey, 1867- ; v. 32- include Review of the mineral production of India, 1898/1903- ; v. 75 consists of Professional papers, no. 1-16; v. 76 consists of Bulletins of economic minerals. |
From inside the book
Results 1-3 of 20
Page 38
It could have been formed in the marginal part of coastal marine basin or supratidal coastal sabkha - type environment ( Shearman , 1966 , 1978 ) . At present , the author prefers to denote the possible Nagaur red facies as continental ...
It could have been formed in the marginal part of coastal marine basin or supratidal coastal sabkha - type environment ( Shearman , 1966 , 1978 ) . At present , the author prefers to denote the possible Nagaur red facies as continental ...
Page 42
The foetid ( HS smelling ) limestone was deposited in a restricted / euxenic environment and before diagenesis , the cavities were probably formed by the escape of ( H , S ) gas bubbles . These cavities were in turn filled in with the ...
The foetid ( HS smelling ) limestone was deposited in a restricted / euxenic environment and before diagenesis , the cavities were probably formed by the escape of ( H , S ) gas bubbles . These cavities were in turn filled in with the ...
Page 43
The problem of collapse breccia and nodular anhydrite is that of post- or syn - sedimentary environment . Widely accepted explanation is that it is a post - diagenetic feature in marine environment . But part of it is possibly non ...
The problem of collapse breccia and nodular anhydrite is that of post- or syn - sedimentary environment . Widely accepted explanation is that it is a post - diagenetic feature in marine environment . But part of it is possibly non ...
What people are saying - Write a review
We haven't found any reviews in the usual places.
Other editions - View all
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 grey ground halite Haryana hinge India indicate inlier iron 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