Multichronometric evidence for an in-situ origin of the ultrahigh-pressure metamorphic terrane of Dabieshan, China


Chavagnac, V., Jahn, B., Villa, I.M., Whitehouse, M.J. and Liu, D. (2001) Multichronometric evidence for an in-situ origin of the ultrahigh-pressure metamorphic terrane of Dabieshan, China Journal of Geology, 109, (5), pp. 633-646.

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Description/Abstract

U-Pb zircon data on gneisses indicate a Late Proterozoic protolith at approx. 700 Ma at Bixiling and a Late Archean to Early Proterozoic for the Shuanghe sheet within the ultrahigh-pressure metamorphic terrane of Dabieshan (China). U-Pb zircon and Sm-Nd dates on the gneisses of the Shuanghe sheet constrain a metamorphic peak at approx. 230 Ma. Rb-Sr and 40Ar-39Ar analyses of phengite from five gneisses in the Bixiling Complex yield ages at 198212 Ma, overlapping the 190220-Ma age on eclogites. The host gneisses record a similar metamorphic evolution as the coesite-bearing eclogites since both the peak and the retrograde evolution were contemporaneous. This argues for an in situ tectonic relationship.

Item Type: Article
ISSNs: 0022-1376 (print)
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ePrint ID: 1334
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2001Published
Date Deposited: 16 Apr 2004
Last Modified: 17 Apr 2017 00:12
Further Information:Google Scholar
URI: http://eprints.soton.ac.uk/id/eprint/1334

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