Foreland sedimentation in Himalayan tectonic regime: a relook at the orogenic processWith reference to India. |
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Page 3
Some Ieucogranites of Late Tertiary age have intruded the Higher and the
Tethyan Himalaya. The steep slope of the Higher Himalaya breaks abruptly into
the lower ranges of the Lesser Himalaya towards south, the boundary between
the two ...
Some Ieucogranites of Late Tertiary age have intruded the Higher and the
Tethyan Himalaya. The steep slope of the Higher Himalaya breaks abruptly into
the lower ranges of the Lesser Himalaya towards south, the boundary between
the two ...
Page 316
16.3), (iii) Kasauli in Subathu Depression through Shali Window and beyond
upto the Tethyan Himalaya (Fig. ... 16.2-5) and abrupt breaks in river gradients
from the Higher to the Lesser Himalaya (Valdiya, 1980a; Seeber and Gomitz,
1983, ...
16.3), (iii) Kasauli in Subathu Depression through Shali Window and beyond
upto the Tethyan Himalaya (Fig. ... 16.2-5) and abrupt breaks in river gradients
from the Higher to the Lesser Himalaya (Valdiya, 1980a; Seeber and Gomitz,
1983, ...
Page 333
The mild folding of the lower structural unit of the Lesser Himalaya comprising
Shali and Simla groups of rocks, as already mentioned, is very similar to that of
the present day autochthon. Partially preserved Subathu (Eocene) sediments
below ...
The mild folding of the lower structural unit of the Lesser Himalaya comprising
Shali and Simla groups of rocks, as already mentioned, is very similar to that of
the present day autochthon. Partially preserved Subathu (Eocene) sediments
below ...
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Contents
AGE OF ENSEQS AND RATE OF SEDIMENTATION | 9 |
INTRODUCTION n | 12 |
ENERGY SEQUENCE CORRELATION | 23 |
Copyright | |
15 other sections not shown
Common terms and phrases
Anticline autochthon basement Batwan Enseq Cenozoic Cenozoic succession Chimnun cis-gamet cis-garnet claystone climate colour conglomerates cycle Dagshai deposits Dharmpur Enseq Dharmsala energy sequence classification Enseq Eocene facies field fine first foredeep foreland basin Formation fossils gamet Ganga GARNET Geol geological cross section grain size trend grey heavy mineral group/subgroup Himachal Pradesh Himalayan India Indo-Gangetic Jammu foothills 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 Mohand Murree non-opaque orogenic parautochthon pebble composition Pleistocene plot Potwar quartzite Raiverman red beds reflection Ridge River Sadhot Enseq sandbodies sandstones Sarkaghat sector sedimentary sediments seismic profiles shale siltstone Simla Hills Siwalik smectite stratification Subathu subgroup Surajpur tectonic Tertiary Tethyan thickness Thrust Tibet traverse trend curve unconformities Upper Siwalik Wah Devi Enseq wrench fault zone
Bibliographic information
| Title | Foreland sedimentation in Himalayan tectonic regime: a relook at the orogenic process |
| Author | V. Raiverman |
| Publisher | Bishen Singh Mahendra Pal Singh, 2002 |
| ISBN | 812110291X, 9788121102919 |
| Length | 378 pages |
| Subjects | › › Geology Science / Earth Sciences / Geology |
| Export Citation | BiBTeX EndNote RefMan |