Reaction mechanism for the replacement of calcite by dolomite and siderite: implications for geochemistry, microstructure and porosity evolution during hydrothermal mineralisation

Author:

Pearce Mark A.,Timms Nicholas E.,Hough Robert M.,Cleverley James S.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference45 articles.

1. Austrheim H (1987) Eclogitization of lower crustal granulites by fluid migration through shear zones. Earth Planet Sci Lett 81:221–232. doi: 10.1016/0012-821X(87)90158-0

2. Beach A (1974) Amphibolitization of Scourian granulites. Scott J Geol 10:35–43

3. Bons PD, Elburg MA, Gomez-Rivas E (2012) A review of the formation of tectonic veins and their microstructures. J Struct Geol 43:33–62. doi: 10.1016/j.jsg.2012.07.005

4. Carey ML (1994) Petrography and geochemistry of selected sills from the Kambalda–Kalgoorlie region, WA. BSc (Hons) thesis, Australian National University, Canberra (unpubl.)

5. Carver RN, Brand NW, Mazzucchelli RH, Kelly GR (2004) Junction Gold Deposit, St Ives District, Western Australia. In: Butt CM, Cornelius M, Scott KM, Robertson IDM (eds) Regolith expression of Australian ore systems. CRC LEME. Available at: http://crcleme.org.au/RegExpOre/Junction.pdf

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