Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic ProcessWith reference to India. |
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Page 166
... sandbodies are single storied . Large trees grew on overbank deposits and these were the first victims of migratory channels which incorporated the fallen trunks in the basal part of the sandstones . Multistoried sandbodies represent ...
... sandbodies are single storied . Large trees grew on overbank deposits and these were the first victims of migratory channels which incorporated the fallen trunks in the basal part of the sandstones . Multistoried sandbodies represent ...
Page 176
... sandbodies . The individual stories , when fully preserved show upward grading from sand to silt or clay , but quite often an upper story rests over the lower one with an erosional contact . The base of a story is often marked by shale ...
... sandbodies . The individual stories , when fully preserved show upward grading from sand to silt or clay , but quite often an upper story rests over the lower one with an erosional contact . The base of a story is often marked by shale ...
Page 177
... sandbodies belonging to five enseqs from Kumarhatti ( upper part ) to Sadhot ( lower part ) . Bed strike and current azimuth rose diagrams indicate that current direction was nearly constant for the time range covered by these enseqs ...
... sandbodies belonging to five enseqs from Kumarhatti ( upper part ) to Sadhot ( lower part ) . Bed strike and current azimuth rose diagrams indicate that current direction was nearly constant for the time range covered by these enseqs ...
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