Foreland sedimentation in Himalayan tectonic regime: a relook at the orogenic processWith reference to India. |
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Page 17
Palynologically it has been dated as Oligocene-Early Miocene (Mathur, 1984).
However, in the inner part of Kangra Depression its upper age limit is much
younger, namely, Late Miocene. Tiwari (1990) has reported Late Miocene
rhizomyid ...
Palynologically it has been dated as Oligocene-Early Miocene (Mathur, 1984).
However, in the inner part of Kangra Depression its upper age limit is much
younger, namely, Late Miocene. Tiwari (1990) has reported Late Miocene
rhizomyid ...
Page 18
On the basis of vertebrate fossils (Pilgrim, 1910; Pascoe, 1964) Nagri has been
assigned a Late Miocene age. Magnetostratigraphy places it between 10.8 and
8.5 m.y.. i.e., Late Miocene (Johnson et al., I985). Dhok Pathan derived its name ...
On the basis of vertebrate fossils (Pilgrim, 1910; Pascoe, 1964) Nagri has been
assigned a Late Miocene age. Magnetostratigraphy places it between 10.8 and
8.5 m.y.. i.e., Late Miocene (Johnson et al., I985). Dhok Pathan derived its name ...
Page 248
EARLY MIOCENE j>'.'?.-, - EARLY oueocemz """'2° 29 ' 'Q 3 4 \5 Potno 0 lS0km
Fig. l2.8(a): lso-frequency plots of cis-garnet heavy minerals in the fold belt and
the foredeep for five enseqs (Kumarhatti. Makreri. explanation to the evolution of
...
EARLY MIOCENE j>'.'?.-, - EARLY oueocemz """'2° 29 ' 'Q 3 4 \5 Potno 0 lS0km
Fig. l2.8(a): lso-frequency plots of cis-garnet heavy minerals in the fold belt and
the foredeep for five enseqs (Kumarhatti. Makreri. explanation to the evolution of
...
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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 |