Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic ProcessWith reference to India. |
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Page 160
... siltstone and claystone , parallel stratification : Sandstone , very fine grained , siltstone and claystone , parallel stratification : Sandstone , very fine to coarse grained , and siltstone , cross bedding : Sandstone , very fine to ...
... siltstone and claystone , parallel stratification : Sandstone , very fine grained , siltstone and claystone , parallel stratification : Sandstone , very fine to coarse grained , and siltstone , cross bedding : Sandstone , very fine to ...
Page 161
... siltstone ( Sh - 1 ) on top of the sandstone unit 4 changes colour upward from grey to red with an uneven zone of colour transition indicating in - situ oxidation . The red siltstone is capped by a grey siltstone ( Sh - 2 ) with sharp ...
... siltstone ( Sh - 1 ) on top of the sandstone unit 4 changes colour upward from grey to red with an uneven zone of colour transition indicating in - situ oxidation . The red siltstone is capped by a grey siltstone ( Sh - 2 ) with sharp ...
Page 175
... siltstone and claystone . Sandstones are very fine grained . Foresets are cross - laminated . ( b ) : Ball and ... siltstone ) passes laterally into facies G ( cross - laminated ) . Another interesting feature is the common occurrence of ...
... siltstone and claystone . Sandstones are very fine grained . Foresets are cross - laminated . ( b ) : Ball and ... siltstone ) passes laterally into facies G ( cross - laminated ) . Another interesting feature is the common occurrence of ...
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