Foreland Sedimentation in Himalayan Tectonic Regime: A Relook at the Orogenic ProcessWith reference to India. |
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Page 96
... fossils of Mid . Eocene age . The maximum duration of this enseq is thus limited to 23.6 m.y. ( 63.6 - 40 23.6 m.y. ) . Kumarhatti Enseq - Compared to Dharmpur , fossils are rarer in this enseq . Palynofossils obtained from a part of ...
... fossils of Mid . Eocene age . The maximum duration of this enseq is thus limited to 23.6 m.y. ( 63.6 - 40 23.6 m.y. ) . Kumarhatti Enseq - Compared to Dharmpur , fossils are rarer in this enseq . Palynofossils obtained from a part of ...
Page 162
... FOSSILS AND PLANT REMAINS Very little studies have been made on trace fossils in the Cenozoic sediments of the Himalayan foothills ( Singh and Sudan , 1997 ) . Trace fossils comprise pipe- like structures , straight and curved or curled ...
... FOSSILS AND PLANT REMAINS Very little studies have been made on trace fossils in the Cenozoic sediments of the Himalayan foothills ( Singh and Sudan , 1997 ) . Trace fossils comprise pipe- like structures , straight and curved or curled ...
Page 166
... fossils consists of finely divided , flaky and dusty carbonized particles . They occur in finely laminated strata , preferably in coarser sediments ranging in texture from very fine to medium grained sandstone . Plant fossils of any ...
... fossils consists of finely divided , flaky and dusty carbonized particles . They occur in finely laminated strata , preferably in coarser sediments ranging in texture from very fine to medium grained sandstone . Plant fossils of any ...
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