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Sediment transport direction in fluviatile Karharbari sandstone, Giridih Basin, Bihar

Abstract

The sandstone is pebbly, very coarse grained in the lower part, and coarse to medium grained in the upper part. Shale and coal respectively constitute 9 and 5% of the strata Small and large erosional channels and successive sets of large scale cross-bedding characterize the sandstone. Palaeo- currents reveal that the paleodrainage and sediment transport were dominantly directed from SSW to NNE.
Publication Date:
Jan 01, 1978
Product Type:
Journal Article
Reference Number:
EDB-80-093560
Resource Relation:
Journal Name: Indian J. Earth Sci.; (India); Journal Volume: 5:1
Subject:
01 COAL, LIGNITE, AND PEAT; COAL SEAMS; GEOLOGIC STRUCTURES; SANDSTONES; SEDIMENTATION; COAL DEPOSITS; GEOLOGIC STRATA; GEOLOGY; INDIA; SHALES; ASIA; DEVELOPING COUNTRIES; GEOLOGIC DEPOSITS; RESOURCES; ROCKS; SEDIMENTARY ROCKS; 011000* - Coal, Lignite, & Peat- Reserves, Geology, & Exploration
OSTI ID:
5231523
Country of Origin:
India
Language:
English
Other Identifying Numbers:
Journal ID: CODEN: IJEAB
Submitting Site:
CLA
Size:
Pages: 95-101
Announcement Date:
May 01, 1980

Citation Formats

Tewari, R C, and Casshyap, S M. Sediment transport direction in fluviatile Karharbari sandstone, Giridih Basin, Bihar. India: N. p., 1978. Web.
Tewari, R C, & Casshyap, S M. Sediment transport direction in fluviatile Karharbari sandstone, Giridih Basin, Bihar. India.
Tewari, R C, and Casshyap, S M. 1978. "Sediment transport direction in fluviatile Karharbari sandstone, Giridih Basin, Bihar." India.
@misc{etde_5231523,
title = {Sediment transport direction in fluviatile Karharbari sandstone, Giridih Basin, Bihar}
author = {Tewari, R C, and Casshyap, S M}
abstractNote = {The sandstone is pebbly, very coarse grained in the lower part, and coarse to medium grained in the upper part. Shale and coal respectively constitute 9 and 5% of the strata Small and large erosional channels and successive sets of large scale cross-bedding characterize the sandstone. Palaeo- currents reveal that the paleodrainage and sediment transport were dominantly directed from SSW to NNE.}
journal = []
volume = {5:1}
journal type = {AC}
place = {India}
year = {1978}
month = {Jan}
}