Foreland sedimentation in Himalayan tectonic regime: a relook at the orogenic processWith reference to India. |
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Page 86
On the basis of palynofossils and vertebrate fossils this enseq has been assigned
a Late Oligocene-Early Miocene age. J AWALAMUKHI ENSEQ This enseq is
named after the temple town of Jawalamukhi (3 l°52'N, 76°l9'E) in the Kangra ...
On the basis of palynofossils and vertebrate fossils this enseq has been assigned
a Late Oligocene-Early Miocene age. J AWALAMUKHI ENSEQ This enseq is
named after the temple town of Jawalamukhi (3 l°52'N, 76°l9'E) in the Kangra ...
Page 128
This time interval covers three enseqs - Jawalamukhi, Kalidhar and Sadhot.
Jawalamukhi Enseq, deposited in a regressive phase, is characterised by a
thickness minima (Fig. 6.1), but hiatuses are rare with this enseq within the fold
belt.
This time interval covers three enseqs - Jawalamukhi, Kalidhar and Sadhot.
Jawalamukhi Enseq, deposited in a regressive phase, is characterised by a
thickness minima (Fig. 6.1), but hiatuses are rare with this enseq within the fold
belt.
Page 129
Anticline, subthrust block of Jawalamukhi Thrust (traverse No. 3, Fig. 7.13). The
Sadhot Enseq is 1859 m thick at Sarkaghat, 823 m at Jawalamukhi and I067 m at
Chakki Khad. Notice that the brownish red coloured conglomerates in the middle
...
Anticline, subthrust block of Jawalamukhi Thrust (traverse No. 3, Fig. 7.13). The
Sadhot Enseq is 1859 m thick at Sarkaghat, 823 m at Jawalamukhi and I067 m at
Chakki Khad. Notice that the brownish red coloured conglomerates in the middle
...
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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 |