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Postgraduate Thesis: Metamorphism of the Helanshan-Qianlishan Complex and its implications for tectonic evolution of the Khondalite Belt in the western block,North China Craton
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TitleMetamorphism of the Helanshan-Qianlishan Complex and its implications for tectonic evolution of the Khondalite Belt in the western block,North China Craton
 
AuthorsYin, Changqing.
尹常青.
 
Issue Date2010
 
PublisherThe University of Hong Kong (Pokfulam, Hong Kong)
 
AdvisorsZhao, G
Sun, M
 
DegreeDoctor of Philosophy
 
SubjectPlate tectonics - China - Ningxia Huizu Zizhiqu.
Geology, Stratigraphic - China - Ningxia Huizu Zizhiqu.
Geology, Structural - China - Ningxia Huizu Zizhiqu.
Cratons - China - Ningxia Huizu Zizhiqu.
 
Dept/ProgramEarth Sciences
 
DOIhttp://dx.doi.org/10.5353/th_b4569899
 
DC FieldValue
dc.contributor.advisorZhao, G
 
dc.contributor.advisorSun, M
 
dc.contributor.authorYin, Changqing.
 
dc.contributor.author尹常青.
 
dc.date.hkucongregation2011
 
dc.date.issued2010
 
dc.description.naturepublished_or_final_version
 
dc.description.thesisdisciplineEarth Sciences
 
dc.description.thesisleveldoctoral
 
dc.description.thesisnameDoctor of Philosophy
 
dc.identifier.doihttp://dx.doi.org/10.5353/th_b4569899
 
dc.identifier.hkulb4569899
 
dc.languageeng
 
dc.publisherThe University of Hong Kong (Pokfulam, Hong Kong)
 
dc.relation.ispartofHKU Theses Online (HKUTO)
 
dc.rightsThe author retains all proprietary rights, (such as patent rights) and the right to use in future works.
 
dc.rightsCreative Commons: Attribution 3.0 Hong Kong License
 
dc.source.urihttp://hub.hku.hk/bib/B45698995
 
dc.subject.lcshPlate tectonics - China - Ningxia Huizu Zizhiqu.
 
dc.subject.lcshGeology, Stratigraphic - China - Ningxia Huizu Zizhiqu.
 
dc.subject.lcshGeology, Structural - China - Ningxia Huizu Zizhiqu.
 
dc.subject.lcshCratons - China - Ningxia Huizu Zizhiqu.
 
dc.titleMetamorphism of the Helanshan-Qianlishan Complex and its implications for tectonic evolution of the Khondalite Belt in the western block,North China Craton
 
dc.typePG_Thesis
 
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