The geology of the Teheran plain

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ID: 293167
1955
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Abstract
Distinguishes and describes four units in the late Tertiary and Quaternary alluvial deposits of the Teheran region in the north Iran plateau, and discusses the provenance of the sediments, the nature and extent of folding and faulting in the older beds, and the occurrence and quality of ground waters in gravels of the Hezardareh formation, the oldest and most extensively developed of the units, believed to be correlative with the Mio-Pliocene Bakhtiari beds of the oil-field region of Iran.
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openalex_W2329942120 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors H. Rieben
Journal american journal of science
Year 1955
DOI
10.2475/ajs.253.11.617
URL
https://ajs.scholasticahq.com/article/58536.pdf
Keywords Keywords not found

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