Original paper

An Early Neoproterozoic Accretionary Prism Ophiolitic Mélange from the Western Jiangnan Orogenic Belt, South China

Volume: 124, Issue: 5, Pages: 587 - 601
Published: Sep 1, 2016
Abstract
The Neoproterozoic Jiangnan orogenic belt delineates the suture zone between the Cathaysia and Yangtze blocks of the South China Craton. The western part of the belt, in the Longsheng region, consists of a disrupted mafic-ultramafic assemblage of pillow basalt, gabbro, diabase, and peridotite along with siliceous marble, ophicalcite, and jasper mixed with basalt. Significant talc deposits occur on the margins of the ultramafic bodies as well as...
Paper Details
Title
An Early Neoproterozoic Accretionary Prism Ophiolitic Mélange from the Western Jiangnan Orogenic Belt, South China
Published Date
Sep 1, 2016
Volume
124
Issue
5
Pages
587 - 601
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