Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic ProcessWith reference to India. |
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Page 19
... conglomerates with assorted pebbles derived from igneous , metamorphic and sedimentary sources , and subordinate sandstones and siltstones . Subsequent workers have noticed that the Boulder Conglomerates are time - transgressive and in ...
... conglomerates with assorted pebbles derived from igneous , metamorphic and sedimentary sources , and subordinate sandstones and siltstones . Subsequent workers have noticed that the Boulder Conglomerates are time - transgressive and in ...
Page 87
... conglomerates laterally giving place to sandstone - shale alternation . The conglomerates of the Sadhot Enseq were deposited by trunk river channels while the interfleuve areas received sandy and shaly deposits . Coalescing ...
... conglomerates laterally giving place to sandstone - shale alternation . The conglomerates of the Sadhot Enseq were deposited by trunk river channels while the interfleuve areas received sandy and shaly deposits . Coalescing ...
Page 182
... conglomerates of Sadhot had been deposited . Such conglomerates outcropping in different parts of the foothills fold belt show close proximity to the major Himalayan rivers like Indus , Ravi , Chenab , Beas , Yamuna , etc. which suggest ...
... conglomerates of Sadhot had been deposited . Such conglomerates outcropping in different parts of the foothills fold belt show close proximity to the major Himalayan rivers like Indus , Ravi , Chenab , Beas , Yamuna , etc. which suggest ...
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