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Goel, R. K.
- Palaeocurrent Analysis of the Siwaliks of Panjab, Haryana and Himachal Pradesh
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Authors
Affiliations
1 Department of Geology & Geophysics, University of Roorkee, Roorkee, U. P., IN
1 Department of Geology & Geophysics, University of Roorkee, Roorkee, U. P., IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 16, No 3 (1975), Pagination: 337-348Abstract
The present paper deals with a study of thickness of cross-bedding units and palaeocurrents as deduced from cross-bedding foreset dip azimuths of the Siwaliks of Panjab, Haryana and Himachal Pradesh. All the three sub-divisions of the Siwaliks-Lower, Middle and Upper exhibit mainly southerly palaeocurrent directions and the variance of cross-bedding foreset dip azimuths seems to decrease from the Lower to Upper Siwaliks. Consistent southerly paleocurrent direction in the Upper Siwaliks suggests that they were probably deposited in a single continuous basin instead of two separate basins.- The Spiti Ordovician-Silurian Succession
Abstract Views :194 |
PDF Views:173
Authors
R. K. Goel
1,
N. G. K. Nair
1
Affiliations
1 Dept. of Geology & Geophysics, University of Roorkee, IN
1 Dept. of Geology & Geophysics, University of Roorkee, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 18, No 1 (1977), Pagination: 47-48Abstract
Classic pin valley section in Spiti (Himachal Pradesh) India, has been re-examined and formal stratigraphic nomenclature in terms of the Lower Paleozoic succession of Spiti is proposed.- Paleogeographic Evolution of a Part of the Indo-Gangetic Trough from the Late Tertiary to Recent
Abstract Views :198 |
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Authors
B. Parkash
1,
R. K. Goel
1
Affiliations
1 Department of Geology and Geophysics, University of Roorkee, Roorkee, U.P., IN
1 Department of Geology and Geophysics, University of Roorkee, Roorkee, U.P., IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 18, No 6 (1977), Pagination: 288-294Abstract
Synthesis of the stratigraphy, paleocurrents and depositional environment of the Siwaliks and sediments suggests that Lower and Middle Siwaliks were deposited predominantly in the form of overlapping, mega alluvial cones of rivers emerging from the Himalaya and flowing southward. Forerunners of some of the modern rivers of great antiquity played an important role in their deposition. During the Upper Siwalik times the Himalaya attained great heights and several important rivers developed on the southern slopes of the central range and deposition continued as before with the difference that a wide piedmont deposit of coarse conglomerate formed near the foot hills. During Siwalik times, an easterly flowing river close to the southern boundary of the area of deposition drained the rivers emerging from the Himalaya.The present geomorphic set up is essentially a continuation of the one developed during Siwalik times with only minor changes.