Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic ProcessWith reference to India. |
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Page 124
... unconformities . LATE EOCENE - EARLY MIOCENE UNCONFORMITIES Unconformities of this period are associated with the early stage of foreland basin sedimentation after the withdrawal of the Eocene sea from the fold belt , covering two ...
... unconformities . LATE EOCENE - EARLY MIOCENE UNCONFORMITIES Unconformities of this period are associated with the early stage of foreland basin sedimentation after the withdrawal of the Eocene sea from the fold belt , covering two ...
Page 128
... UNCONFORMITIES ยท This period has the least number of unconformities . This time interval covers three enseqs - Jawalamukhi , Kalidhar and Sadhot . Jawalamukhi Enseq , deposited in a regressive phase , is characterised by a thickness ...
... UNCONFORMITIES ยท This period has the least number of unconformities . This time interval covers three enseqs - Jawalamukhi , Kalidhar and Sadhot . Jawalamukhi Enseq , deposited in a regressive phase , is characterised by a thickness ...
Page 136
... unconformities both in time and space within the foreland basin . The major unconformities are marked by the complete absence of one or more than one enseqs in some subbasins . But there are other unconformities where certain enseqs are ...
... unconformities both in time and space within the foreland basin . The major unconformities are marked by the complete absence of one or more than one enseqs in some subbasins . But there are other unconformities where certain enseqs are ...
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