File Download

There are no files associated with this item.

  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Formation of podiform chromitites by melt/rock interaction in the upper mantle

TitleFormation of podiform chromitites by melt/rock interaction in the upper mantle
Authors
Issue Date1994
PublisherSpringer Verlag. The Journal's web site is located at http://link.springer.de/link/service/journals/00126/index.htm
Citation
Mineralium Deposita, 1994, v. 29 n. 1, p. 98-101 How to Cite?
AbstractHigh-Cr and high-Al podiform chromitites are derived from melts formed by high and low degrees of partial melting in the upper mantle, respectively. The close association of the chromitites, regardless of compositions, with dunites and harzburgites can be explained by interaction between melts and harzburgites or depleted lherzolites in the upper mantle. Continuous reaction between melt and wallrock modifies the compositions of the magmas towards the precipitation of chromite alone under upper mantle conditions. The modified magmas would have higher silica and lower magnesia and would be extracted into the crust or erupted, leaving chromite pods in situ with dunite rinds that grade to harzburgites or lherzolites. -Authors
Persistent Identifierhttp://hdl.handle.net/10722/150963
ISSN
2015 Impact Factor: 3.467
2015 SCImago Journal Rankings: 1.677

 

DC FieldValueLanguage
dc.contributor.authorZhou, MFen_US
dc.contributor.authorRobinson, PTen_US
dc.contributor.authorBai, WJen_US
dc.date.accessioned2012-06-26T06:15:18Z-
dc.date.available2012-06-26T06:15:18Z-
dc.date.issued1994en_US
dc.identifier.citationMineralium Deposita, 1994, v. 29 n. 1, p. 98-101en_US
dc.identifier.issn0026-4598en_US
dc.identifier.urihttp://hdl.handle.net/10722/150963-
dc.description.abstractHigh-Cr and high-Al podiform chromitites are derived from melts formed by high and low degrees of partial melting in the upper mantle, respectively. The close association of the chromitites, regardless of compositions, with dunites and harzburgites can be explained by interaction between melts and harzburgites or depleted lherzolites in the upper mantle. Continuous reaction between melt and wallrock modifies the compositions of the magmas towards the precipitation of chromite alone under upper mantle conditions. The modified magmas would have higher silica and lower magnesia and would be extracted into the crust or erupted, leaving chromite pods in situ with dunite rinds that grade to harzburgites or lherzolites. -Authorsen_US
dc.languageengen_US
dc.publisherSpringer Verlag. The Journal's web site is located at http://link.springer.de/link/service/journals/00126/index.htmen_US
dc.relation.ispartofMineralium Depositaen_US
dc.titleFormation of podiform chromitites by melt/rock interaction in the upper mantleen_US
dc.typeArticleen_US
dc.identifier.emailZhou, MF:mfzhou@hkucc.hku.hken_US
dc.identifier.authorityZhou, MF=rp00844en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.scopuseid_2-s2.0-0028197728en_US
dc.identifier.volume29en_US
dc.identifier.issue1en_US
dc.identifier.spage98en_US
dc.identifier.epage101en_US
dc.publisher.placeGermanyen_US
dc.identifier.scopusauthoridZhou, MF=7403506005en_US
dc.identifier.scopusauthoridRobinson, PT=7403720506en_US
dc.identifier.scopusauthoridBai, WJ=9271474700en_US

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats