LOWER ECCA SHALE D . T . A . CURVES - A THERMO - DY NAMlC INTERPRETATION
نویسنده
چکیده
Typical D.T.A. peak systems yielded by the fresh lower Ecca shales in the Durban and Pietermaritzburg areas are presented. The theoretical course of recrystallisation for these rocks is derived from chemical thermodynamic data. These theoretical results agree well with experimental observation. Carbon is found to dictate the course of recrystallisation on the basis of overall chemical rather than detailed mineralogical composition.
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