Petrology of the mafic rocks of the Xigaze ophiolite, Tibet View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1985-08

AUTHORS

Jacques Girardeau, Jean Claude C Mercier, Wang Xibin

ABSTRACT

The Xigaze ophiolite (Yarlung-Zangbo suture zone, Southern Tibet, China) shows an unusual crustal sequence characterized by a lack of large masses of cumulate gabbros, by dolerites intrusive throughout the whole ophiolite sequence, and by the injection of dolerites in already serpentinized peridotites. The abyssal tholeiitic nature of all the mafic rocks indicates that they have been generated at an oceanic ridge. All the geological arguments and petrological and textural data on the mafic rocks point to very low heat production and large heat losses through widespread intensive sea-water circulation, for the spreading centre in which they have been formed, in good agreement with a slow-spreading ridge origin. More... »

PAGES

309-321

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/bf00384710

DOI

http://dx.doi.org/10.1007/bf00384710

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1019631575


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