نتایج جستجو برای: metamorphism

تعداد نتایج: 2072  

Journal: :Transactions of the Edinburgh Geological Society 1897

M. Jamshidi Badr

Soursat Metamorphic Complex (SMC) in west of Takab city is one of the polyphase metamorphic terrenes in northern Sanandaj-Sirjan metamorphic belt of Iran. The SMC composed mainly of metasedimentary rocks associated with granitic intrusions. Based on metamorphic rocks, two metamorphic phases could be separate in the complex. M1 is representative of regional metamorphisms which varies from greens...

2006
P. BAYLISS A. A. LEVINSON

Dolomite or calcite, quartz and kaolinite in various proportions were reacted at 250-300~ temperatures and pressures up to 90 bars in a hydrous environment. Reactions which approached completion produced talc, calcite, montmorillonite, anorthite (both metastable hexagonal and stable triclinic polymorphs) and the rare Ca-zeolite, garronite. These reactions are applicable to diagenesis, low-grade...

2005
METAMORPHISM. A. Zhang W. Hsu R. Wang M. Ding

SHOCKED SIXIANGKOU L6 CHONDRITE: FURTHER CONSTRAINTS ON CONDITIONS OF SHOCK METAMORPHISM. A. Zhang , W. Hsu, R. Wang, and M. Ding, 1 Laboratory for Astrochemistry and Planetary Sciences, Purple Mountain Observatory, Chinese Academy of Sciences, Nanjing 210008, China, [email protected], [email protected], [email protected], 2 State Key Laboratory for Mineral Deposits Research and Department of Ea...

Journal: :journal of sciences, islamic republic of iran 2010
m. jamshidi badr

soursat metamorphic complex (smc) in west of takab city is one of the polyphase metamorphic terrenes in northern sanandaj-sirjan metamorphic belt of iran. the smc composed mainly of metasedimentary rocks associated with granitic intrusions. based on metamorphic rocks, two metamorphic phases could be separate in the complex. m1 is representative of regional metamorphisms which varies from greens...

Journal: :The Journal of the Geological Society of Japan 1969

Journal: :The Journal of the Geological Society of Japan 1958

Journal: :Journal of Geophysical Research 1964

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