Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic ProcessWith reference to India. |
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Page 12
... Dagshai to Kasauli Formation in the Bilaspur structural unit ( west of Surajpur Thrust ) and their interfingering relation in the Surajpur structural unit ( east of Surajpur Thrust ) . There is an unconformity between Subathu and Dagshai ...
... Dagshai to Kasauli Formation in the Bilaspur structural unit ( west of Surajpur Thrust ) and their interfingering relation in the Surajpur structural unit ( east of Surajpur Thrust ) . There is an unconformity between Subathu and Dagshai ...
Page 13
... DAGSHAI FORMATION Named after the Dagshai Cantonment in the Simla Hills , the Dagshai Formation predominantly consists of red coloured shales , often with calcareous concretions , and sandstones of brown and steel - grey colour . It has ...
... DAGSHAI FORMATION Named after the Dagshai Cantonment in the Simla Hills , the Dagshai Formation predominantly consists of red coloured shales , often with calcareous concretions , and sandstones of brown and steel - grey colour . It has ...
Page 16
... Dagshai are as old as the basal Subathu ( Late Paleocene - Eocene ) by virtue of their interfingering relation with the latter . What is the upper age limit of Dagshai ? Should the age of the 500 m thick Dagshai beds near Subathu ( Fig ...
... Dagshai are as old as the basal Subathu ( Late Paleocene - Eocene ) by virtue of their interfingering relation with the latter . What is the upper age limit of Dagshai ? Should the age of the 500 m thick Dagshai beds near Subathu ( Fig ...
Contents
INTRODUCTION | 1 |
STRATIGRAPHY | 9 |
ENERGY SEQUENCE CORRELATION | 23 |
Copyright | |
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Common terms and phrases
Anticline autochthon basement Batwan Enseq Beas Beas River Cenozoic Chenab Chimnun cis-garnet clastics claystone climate colour conglomerates cycle Dagshai Dehradun deposits Dharmpur Enseq Dharmsala energy sequence classification Enseq Eocene facies fold belt foothills foreland basin Formation fossils frequency Gandak Ganga GARNET Geol geological cross section grain size trend gravels grey heavy minerals Himalaya India Indo-Gangetic Foredeep Jammu Jawalamukhi Jawalamukhi Enseq Kalidhar Enseq Kangra Kangra Depression Kasauli Khad Kumar Kumarhatti Enseq Lesser Himalaya limestone Lithology location in Fig Makreri Enseq Middle Siwalik Miocene Murree opaque orogenic parautochthon pebble composition Pleistocene Potwar PRE-TERTIARY PT PT quartzite Raiverman Ravi red beds Ridge River Sadhot Enseq sandbodies sandstones Sarda Enseq Sarkaghat sector sedimentary sediments seismic profiles shale shows siltstone Siwalik smectite stratification stratigraphic strike-slip structural Sub-Himalaya Subathu Subathu Depression Syncline tectonic Tertiary Tethyan thickness Tibet traverse trend curve unconformity uplift Upper Siwalik Wah Devi Enseq wrench fault zone