Foreland sedimentation in Himalayan tectonic regime: a relook at the orogenic processWith reference to India. |
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Page 29
It is well illustrated in the case of energy sequence plots of three sections: Guma,
BirdharChimnun and Sarkaghat (Fig. 3.4). From north (Guma) to south (
Sarkaghat) these sections belong to the same tectonic province and the same ...
It is well illustrated in the case of energy sequence plots of three sections: Guma,
BirdharChimnun and Sarkaghat (Fig. 3.4). From north (Guma) to south (
Sarkaghat) these sections belong to the same tectonic province and the same ...
Page 129
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 part of Sadhot at Sarkaghat are missing at Jawalamukhi, but they are ...
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 part of Sadhot at Sarkaghat are missing at Jawalamukhi, but they are ...
Page 155
Table 9.1: Thickness Frequency Distribution (A) Plane stratification (thickness
scale as in Table 9.2, data from Dhannpur to Kalidhar enseqs of Chimnun
traverse and from Kumarhatti to Kalidhar enseqs of Sarkaghat traverse).
Thickness scale I ...
Table 9.1: Thickness Frequency Distribution (A) Plane stratification (thickness
scale as in Table 9.2, data from Dhannpur to Kalidhar enseqs of Chimnun
traverse and from Kumarhatti to Kalidhar enseqs of Sarkaghat traverse).
Thickness scale I ...
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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 |