Possible source dichotomy of contemporaneous post-collisional barren I-type versus tin-bearing A-type granites, lying on opposite sides of the South Tien Shan suture

Ore Geology Reviews

Volumn 35, Issue 2, 2009, Pages 206-216

  Konopelko, Dmitry ^a   Seltmann, Reimar ^b   Biske, Georgy ^a   Lepekhina, Elena ^c   Sergeev, Sergei ^c  

^a ST PETERSBURG STATE UNIVERSITY   (Russian Federation)

^b DEPARTMENT OF LIFE SCIENCES   (United Kingdom)

^c A P KARPINSKY RUSSIAN GEOLOGICAL RESEARCH INSTITUTE   (Russian Federation)

Author keywords

A type granite; I type granite; Shear zone; Suture; Tien Shan; U Pb geochronology

Indexed keywords

A-TYPE GRANITE; I-TYPE GRANITE; SHEAR ZONE; SUTURE; TIEN SHAN; U-PB GEOCHRONOLOGY;

ANALYTICAL GEOCHEMISTRY; BORON; BORON COMPOUNDS; GEOCHRONOLOGY; LEAD ALLOYS; MINERALOGY; OCEAN ENGINEERING; OCEANOGRAPHY; POTASSIUM; SILICATE MINERALS; TIN; TITANIUM COMPOUNDS; TRACE ANALYSIS; ZIRCON;

GRANITE;

A-TYPE ROCK; CALC ALKALINE ROCK; CONTINENTAL COLLISION; GRANITOID; I-TYPE ROCK; METALLOGENESIS; MINERALIZATION; PASSIVE MARGIN; PRECAMBRIAN; SHEAR ZONE; SHRIMP DATING; SUTURE ZONE; TIN; URANIUM-LEAD DATING; ZIRCON;

ASIA; CHINA; EURASIA; FAR EAST; TARIM BASIN; TIEN SHAN; XINJIANG UYGUR;

EID: 63649153410     PISSN: 01691368     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.oregeorev.2009.01.002     Document Type: Article

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