Age of the Holenarsipur Greenstone Belt, relationships with the surrounding gneisses (Karnataka, south India)

dc.contributor.author Peucat, J. J.
dc.contributor.author Bouhallier, H.
dc.contributor.author Fanning, C. M.
dc.contributor.author Jayananda, M.
dc.date.accessioned 2022-03-26T23:51:19Z
dc.date.available 2022-03-26T23:51:19Z
dc.date.issued 1995-01-01
dc.description.abstract A rhyolitic volcanic flow included in the Holenarsipur greenstone belt, has a simple igneous population of zircons which has a SHRIMP 207Pb/206Pb age of 3298 ± 7 Ma, interpreted as the crystallization age of this flow and considered synchroneous with deposition of the coeval sedimentary pile. The Holenarsipur greenstone belt is now documented as the oldest supracrustal accumulation in the Dharwar craton. From field and other published geochronological results it is concluded that a large part of the surrounding gneisses are very close in age to this rhyolite. -from Authors
dc.identifier.citation Journal of Geology. v.103(6)
dc.identifier.issn 00221376
dc.identifier.uri 10.1086/629789
dc.identifier.uri https://www.journals.uchicago.edu/doi/10.1086/629789
dc.identifier.uri https://dspace.uohyd.ac.in/handle/1/2821
dc.title Age of the Holenarsipur Greenstone Belt, relationships with the surrounding gneisses (Karnataka, south India)
dc.type Journal. Article
dspace.entity.type
Files
License bundle
Now showing 1 - 1 of 1
No Thumbnail Available
Name:
license.txt
Size:
1.71 KB
Format:
Plain Text
Description: