Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic ProcessWith reference to India. |
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Page 283
... sector 4 ( Fig . 15.1 ) . It may be noted that the sectors 1-3 belong to the autochthon while the sector 4 to the parautochthon . · Sector 1 This sector includes the autochthon from two subbasins , namely , Naoshera and Ramnagar . The ...
... sector 4 ( Fig . 15.1 ) . It may be noted that the sectors 1-3 belong to the autochthon while the sector 4 to the parautochthon . · Sector 1 This sector includes the autochthon from two subbasins , namely , Naoshera and Ramnagar . The ...
Page 295
... SECTOR I SECTOR 2. THRUSTS AND WRENCH FAULTS The principal compressive stress in the Himalayan tectonic belt is oriented N - S ( Dasgupta et al . , 1987 ; DeMets et al . , 1990 ; Dubey and Bhat , 1991 ) . The stress field in the foreland ...
... SECTOR I SECTOR 2. THRUSTS AND WRENCH FAULTS The principal compressive stress in the Himalayan tectonic belt is oriented N - S ( Dasgupta et al . , 1987 ; DeMets et al . , 1990 ; Dubey and Bhat , 1991 ) . The stress field in the foreland ...
Page 297
... ( Sector 1 ) compared to the SE ( Sector 2 ) . ft x 103 SECTOR 3 AUTOCHTHON Mohand E. MIO -. minimised , well illustrated by the BSM Wrench Fault Zone . This fault zone makes an acute angle , about 45 ° , with the south - directed ...
... ( Sector 1 ) compared to the SE ( Sector 2 ) . ft x 103 SECTOR 3 AUTOCHTHON Mohand E. MIO -. minimised , well illustrated by the BSM Wrench Fault Zone . This fault zone makes an acute angle , about 45 ° , with the south - directed ...
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