doi.org/10.1016/j.epsl.2009.11.044
Original paper

Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: Implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China

J.G. Shellnutt
8
,
Bor-ming Jahn
90
Earth and Planetary Science Letters4.80
Volume: 289, Issue: 3-4, Pages: 509 - 519
Published: Jan 1, 2010
Abstract
The Late Permian (260 Ma) Emeishan large igneous province of SW China contains numerous magmatic Fe–Ti oxide deposits. The Fe–Ti oxide deposits occur in the lower parts of evolved layered gabbroic intrusions which are spatially and temporally associated with A-type granitic rocks. The 260 Ma Panzhihua layered gabbroic intrusion hosts one of the largest magmatic Fe–Ti oxide deposits in China and is coeval with a peralkaline A-type granitic...
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Paper Details
Title
Formation of the Late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: Implications for the genesis of Fe–Ti oxide deposits and A-type granites of SW China
DOI
doi.org/10.1016/j.epsl.2009.11.044
Published Date
Jan 1, 2010
Journal
Earth and Planetary Science Letters
Volume
289
Issue
3-4
Pages
509 - 519
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