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- W2389788563 abstract "Clinopyroxenes in eclogites from Bixiling and Huangzhen, Dabieshan have been investigated by FTIR. Structural water occurs in all omphacites as hydroxyl (OH~-) with cnntent up to ～2000ppm (H_2O wt.). Water content is heterogeneous on the outcrop (～150m) scale at Bixiling and homogeneous at Huangzheng on the 3km scale, and the distribution characteristics were inherited from their protoliths. The water-rock interaction which Dabieshan eclogites'protoliths experienced was channeled for Bixiling and pervasive for Huangzheng. The protolith of Bixiling eclogites was probably gabbroic intrusion and that of Huangzheng eclogites was probably basalt. Water content of Bixiling clinopyroxenes (1400ppm) was significantly lower than that of Huangzheng clinopyroxenes (～1850ppm), whieh aroses from different protolith and tbe way of water-rock interaction before subduction." @default.
- W2389788563 created "2016-06-24" @default.
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- W2389788563 date "2004-01-01" @default.
- W2389788563 modified "2023-09-25" @default.
- W2389788563 title "Water in clinopyroxenes from eclogites of Bixiling and Huangzheng, Dabicshan and geodynamic implications." @default.
- W2389788563 hasPublicationYear "2004" @default.
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