File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Geology and genesis of the Zhou'an PGE-Cu-Ni deposit, Henan Province

TitleGeology and genesis of the Zhou'an PGE-Cu-Ni deposit, Henan Province
Authors
KeywordsHydrothermal Deposit
Pge-Cu-Ni Deposit
Qinling Orogen
Ultramafic Intrusion
Issue Date2006
Citation
Kuangwu Yanshi, 2006, v. 26 n. 3, p. 31-37 How to Cite?
AbstractThe Zhou'an deposit, containing 0.335 × 106 t Ni, 0.180 6 × 106 t Cu and 33.03 t Pt + Pd, is a large blind PGE-Cu-Ni deposit beneath the Nanyang basin. It is located at the suturing zone between the Yangtze and Sinokorea plates,i. e. the northern margin the Sujiahe Precambrian terrane of the southern Qinling Orogen. The ore-bearing ultramafic complex intruded into the Meso-Neoproterozoic metamorphic strata and was strongly altered. The stratiform-like PGE-Cu-Ni orebodies are hosted in the strongly altered shell surround the inner contact zone of the ultramafic intrusion. They mainly occur on the top or at the bottom of the intrusion. All these characters suggest that the ores were formed by post-magmatism hydrothermal alteration. The most important is that the Zhou'an deposit is the fist case of large-size PGE-Cu-Ni deposit discovered in the Qinling Orogen, which implies that the Qinling Orogen is potential for ore deposits of similar types.
Persistent Identifierhttp://hdl.handle.net/10722/92288
ISSN
2015 SCImago Journal Rankings: 0.169
References

 

DC FieldValueLanguage
dc.contributor.authorWang, J-Men_HK
dc.contributor.authorChen, Y-Jen_HK
dc.contributor.authorLi, S-Ien_HK
dc.contributor.authorWang, G-Men_HK
dc.contributor.authorMei, Men_HK
dc.date.accessioned2010-09-17T10:41:37Z-
dc.date.available2010-09-17T10:41:37Z-
dc.date.issued2006en_HK
dc.identifier.citationKuangwu Yanshi, 2006, v. 26 n. 3, p. 31-37en_HK
dc.identifier.issn1001-6872en_HK
dc.identifier.urihttp://hdl.handle.net/10722/92288-
dc.description.abstractThe Zhou'an deposit, containing 0.335 × 106 t Ni, 0.180 6 × 106 t Cu and 33.03 t Pt + Pd, is a large blind PGE-Cu-Ni deposit beneath the Nanyang basin. It is located at the suturing zone between the Yangtze and Sinokorea plates,i. e. the northern margin the Sujiahe Precambrian terrane of the southern Qinling Orogen. The ore-bearing ultramafic complex intruded into the Meso-Neoproterozoic metamorphic strata and was strongly altered. The stratiform-like PGE-Cu-Ni orebodies are hosted in the strongly altered shell surround the inner contact zone of the ultramafic intrusion. They mainly occur on the top or at the bottom of the intrusion. All these characters suggest that the ores were formed by post-magmatism hydrothermal alteration. The most important is that the Zhou'an deposit is the fist case of large-size PGE-Cu-Ni deposit discovered in the Qinling Orogen, which implies that the Qinling Orogen is potential for ore deposits of similar types.en_HK
dc.languageengen_HK
dc.relation.ispartofKuangwu Yanshien_HK
dc.subjectHydrothermal Depositen_HK
dc.subjectPge-Cu-Ni Depositen_HK
dc.subjectQinling Orogenen_HK
dc.subjectUltramafic Intrusionen_HK
dc.titleGeology and genesis of the Zhou'an PGE-Cu-Ni deposit, Henan Provinceen_HK
dc.typeArticleen_HK
dc.identifier.emailChen, Y:ychenc@hkucc.hku.hken_HK
dc.identifier.authorityChen, Y=rp1318en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.scopuseid_2-s2.0-33751362131en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-33751362131&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume26en_HK
dc.identifier.issue3en_HK
dc.identifier.spage31en_HK
dc.identifier.epage37en_HK

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats