Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic ProcessWith reference to India. |
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Page 5
... autochthon and an inner parautochthon ( Boileau and Kohli , 1952 ; Raiverman et al . , 1993 , 1994b ) . The narrower belt in the east comprises mainly the autochthon unit except in the stretch between Ganga and Sarda rivers where it is ...
... autochthon and an inner parautochthon ( Boileau and Kohli , 1952 ; Raiverman et al . , 1993 , 1994b ) . The narrower belt in the east comprises mainly the autochthon unit except in the stretch between Ganga and Sarda rivers where it is ...
Page 306
... autochthon . Two prominent unconformities , one between Jawalamukhi and Kalidhar enseqs ( Fig . 4.25 ) and the other within the Sadhot Enseq ( Fig . 7.13 ) are known within the Jawalamukhi structural unit suggesting two instances of ...
... autochthon . Two prominent unconformities , one between Jawalamukhi and Kalidhar enseqs ( Fig . 4.25 ) and the other within the Sadhot Enseq ( Fig . 7.13 ) are known within the Jawalamukhi structural unit suggesting two instances of ...
Page 311
... autochthon and parautochthon . The incipient parautochthon witnessed at this time either stoppage of sedimentation due to arrested subsidence , as in the case of the Subathu Depression , or the sedimentation process operated at a much ...
... autochthon and parautochthon . The incipient parautochthon witnessed at this time either stoppage of sedimentation due to arrested subsidence , as in the case of the Subathu Depression , or the sedimentation process operated at a much ...
Contents
INTRODUCTION | 1 |
STRATIGRAPHY | 9 |
ENERGY SEQUENCE CORRELATION | 23 |
Copyright | |
23 other sections not shown
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