Foreland sedimentation in Himalayan tectonic regime: a relook at the orogenic processWith reference to India. |
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Page 82
Kangra Depression in the middle lacks sillimanite but shows sporadic
homblende (see Masdhawan section, Fig. 4.2). Batwan Enseq - Opaque
concentration is high at 7080% and so is cis-gamet. In some sections, opaque
and cis-garnet show ...
Kangra Depression in the middle lacks sillimanite but shows sporadic
homblende (see Masdhawan section, Fig. 4.2). Batwan Enseq - Opaque
concentration is high at 7080% and so is cis-gamet. In some sections, opaque
and cis-garnet show ...
Page 130
-é 9'-'n.o.o. 0 'I; o o ENSEO LIJ ID < 0 10km iii BATWAN MID. PLEIST Congl grey
coloured Limestone pbl and calc. Matrix common. 0pq,Cis. garnet and garnet
frequency variable On 2 0 o '__ - " ' ' O B o 1. '_ .- flea 0 P. -O ~- edbeds A .. -. , go
.
-é 9'-'n.o.o. 0 'I; o o ENSEO LIJ ID < 0 10km iii BATWAN MID. PLEIST Congl grey
coloured Limestone pbl and calc. Matrix common. 0pq,Cis. garnet and garnet
frequency variable On 2 0 o '__ - " ' ' O B o 1. '_ .- flea 0 P. -O ~- edbeds A .. -. , go
.
Page 256
Minimum opaque and cis-gamet, and maximum garnet concentration (Fig. 4.12)
point directly to a cold paleoclimate. Sadhot Enseq (Late Miocene-Early
Pleistocene) is divisible into three parts - lower. middle and upper. Lower and
upper parts ...
Minimum opaque and cis-gamet, and maximum garnet concentration (Fig. 4.12)
point directly to a cold paleoclimate. Sadhot Enseq (Late Miocene-Early
Pleistocene) is divisible into three parts - lower. middle and upper. Lower and
upper parts ...
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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 |