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混合型石棉矿床的基本地质特征

GENERAL GEOLOGICAL CHARACTERISTICS OF A CERTAIN ASBESTOS DEPOSIT, SHAANXI PROVINCE
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摘要 As is evidenced from the occurrence, mineral composition, asbestos minerals, the type of veins and fibrous characters it is recognized that the origin of the asbestos deposit studied in this paper in Shaanxi is different from either the serpentine type resulted from ultrabasic rocks or that originated from dolomitic limestones or dolomite.It can be considered as a gradation between the two types mentioned above. As is evidenced from the occurrence, mineral composition, asbestos minerals, the type of veins and fibrous characters it is recognized that the origin of the asbestos deposit studied in this paper in Shaanxi is different from either the serpentine type resulted from ultrabasic rocks or that originated from dolomitie limestones or dolomite. It can be considered as a gradation between the two types mentioned above.
作者 汪仁勇
出处 《地球化学》 CAS 1982年第1期96-102,共7页 Geochimica
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