Records of the Geological Survey of India, Volume 141, Part 8The Survey, 2006 - Earthquakes Vols. 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. |
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Page 8
... dipping vertical to sub - vertical , ii ) N50 ° W- S50 ° E , dipping 40-50 ° SW and iii ) North - South , dipping 60 ° to 65 ° west . During rains , the strata get fully saturated with water and develop pore pressure resulting into ...
... dipping vertical to sub - vertical , ii ) N50 ° W- S50 ° E , dipping 40-50 ° SW and iii ) North - South , dipping 60 ° to 65 ° west . During rains , the strata get fully saturated with water and develop pore pressure resulting into ...
Page 90
... dipping joint is the most prominent and forms wedge with foliation . Thick overburden and potential structural wedges are the main geotechnical problems . Based on the geological assessment , prima facie all the structures have been ...
... dipping joint is the most prominent and forms wedge with foliation . Thick overburden and potential structural wedges are the main geotechnical problems . Based on the geological assessment , prima facie all the structures have been ...
Page 91
... dipping ( 40 ° -55 ° ) joint ( dipping opposite to each other ) walls are seen as exposed planes under planar failure / toppling . No major geotechnical problem is observed except wedge failure and minor over breaks . In general ...
... dipping ( 40 ° -55 ° ) joint ( dipping opposite to each other ) walls are seen as exposed planes under planar failure / toppling . No major geotechnical problem is observed except wedge failure and minor over breaks . In general ...
Contents
प्रचालन जम्मू एवं कश्मीर द्वारा किए गए कार्यों का विहंगावलोकन | 1 |
Group of rocks in Pithoragarh Nainital Almora and Dehradun districts Uttarakhand | 135 |
Specialised thematic mapping of discontinuities across the lithostratigraphic sections | 141 |
Copyright | |
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