Palaeozoic pre- and post-collision calc-alkaline magmatism in the Qinling orogenic belt, central China, as documented by zircon ages on granitoid rocks

1996 ◽  
Vol 153 (3) ◽  
pp. 409-417 ◽  
Author(s):  
F. XUE ◽  
A. KRÖNER ◽  
T. REISCHMANN ◽  
F. LERCH
Keyword(s):  
Orogenic Belt ◽  
Central China ◽  
Alkaline Magmatism ◽  
Calc Alkaline ◽  
Qinling Orogenic Belt ◽  
Granitoid Rocks

Genesis of the high Sr/Y rocks in Qinling orogenic belt, central China

Lithos ◽  
2018 ◽  
Vol 314-315 ◽  
pp. 337-349 ◽  
Author(s):  
Long Ren ◽  
Huaying Liang ◽  
Zhiwei Bao ◽  
Jian Zhang ◽  
Kaixuan Li ◽  
...  
Keyword(s):  
Orogenic Belt ◽  
Central China ◽  
Qinling Orogenic Belt

Magnetite–apatite intrusions and calc-alkaline magmatism, Camsell River, N.W.T.

1976 ◽  
Vol 13 (2) ◽  
pp. 348-354 ◽  
Author(s):  
J. P. N. Badham ◽  
R. D. Morton
Keyword(s):  
Volcanic Rocks ◽  
Orogenic Belt ◽  
Alkaline Magmatism ◽  
Calc Alkaline ◽  
Immiscible Liquids ◽  
Intermediate Composition ◽  
Andean Type

The Camsell River area comprises a roof pendant of volcanic rocks within an Aphebian (~1800 m.y.) orogenic belt. Magnetite–apatite intrusions and related bodies are common and are closely associated with plutons of intermediate composition. The magnetitic intrusions are interpreted as immiscible liquids that separated from a magma of intermediate composition. The immiscible fractions were predominantly crystalline when they reached their present higher levels, and final emplacement was facilitated by volatile-streaming and fluidization. Their presence in the orogenic belt is taken as further support for the hypothesis that the orogen was of Andean type.

A unique Mo deposit associated with carbonatites in the Qinling orogenic belt, central China

Lithos ◽  
2010 ◽  
Vol 118 (1-2) ◽  
pp. 50-60 ◽  
Author(s):  
Cheng Xu ◽  
Jindrich Kynicky ◽  
Anton R. Chakhmouradian ◽  
Liang Qi ◽  
Wenlei Song
Keyword(s):  
Orogenic Belt ◽  
Central China ◽  
Qinling Orogenic Belt
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