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地质学报  2001 

柴达木盆地北缘都兰地区榴辉岩中透长石+石英包裹体:超高压变质作用的证据

, PP. 180-185

Keywords: 榴辉岩透长石多晶石英包裹体超高压变质作用柴达木盆地变质岩柯石英

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Abstract:

近年来在祁连地体与紫达木地块之间大柴旦--都兰北一线确定出一条榴辉岩带。在此带东端北部地区野马滩一带榴辉岩中,我们发现产在石榴子石内部由透长石和多晶石英(柯石英假像)构成的包裹体。包裹体在内部结构特征及周围的状裂纹反映早期超高压变质相特征,据此,推测柴达木盆地北缘榴辉岩带可能是一形成深度超过80km的超高压变质带。

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