Ni?Cu?(PGE) magmatic sulfide deposits in the Yangliuping area, Permian Emeishan igneous province, SW...
Ni?Cu?(PGE) magmatic sulfide deposits in the Yangliuping area, Permian Emeishan igneous province, SW China
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Publisher
Heidelberg: Springer Nature B.V
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Language
English
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Publisher
Heidelberg: Springer Nature B.V
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Contents
The Ni-Cu-PGE sulfide deposits in the Yangliuping area, SW China, are hosted in mafic-ultramafic sills. The four mineralized sills are located in the Yangliuping tectonic dome and intrude Devonian carbonaceous marble, graphitic schist. The sills are 200-300 m thick and 1,000-2,000 m in strike length and now consist chiefly of serpentinite, talc sch...
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Full title
Ni?Cu?(PGE) magmatic sulfide deposits in the Yangliuping area, Permian Emeishan igneous province, SW China
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TN_cdi_proquest_journals_643609650
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_643609650
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ISSN
0026-4598
E-ISSN
1432-1866
DOI
10.1007/s00126-003-0362-3
