Roy, Supriya ; Purkait, P. K. (1965) Stability relations of manganese oxide minerals in metamorphic orebodies corresponding to sillimanite grade in Gowari Wadhona Mine area, Chhindwara District, Madhya Pradesh, India Economic Geology, 60 (3). pp. 601-613. ISSN 0361-0128
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Official URL: http://economicgeology.org/cgi/content/abstract/60...
Related URL: http://dx.doi.org/10.2113/gsecongeo.60.3.601
Abstract
Paragenesis is determined from textural features involves the following minerals--braunite, hollandite, bixbyite, vredenburgite, jacobsite, hausmannite, manganite, pyrolusite, cryptomelane, and hematite. Identifications were confirmed by X-ray. The stability and transformation of these minerals may be correlated with laboratory phase equilibrium studies, although experimentally determined temperatures seem high, perhaps because carried out in air.
Item Type: | Article |
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Source: | Copyright of this article belongs to Society of Economic Geologists. |
ID Code: | 42602 |
Deposited On: | 04 Jun 2011 13:07 |
Last Modified: | 04 Jun 2011 13:07 |
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