Evidence of isotopic equilibration between microgranitoid enclaves and host granodiorite, Warburton Granodiorite, Lachlan Fold Belt, Australia-Reference-Cited by-同舟云学术

Evidence of isotopic equilibration between microgranitoid enclaves and host granodiorite, Warburton Granodiorite, Lachlan Fold Belt, Australia

Published:1996-07 Issue:1-2 Volume:38 Page:1-22
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Elburg M.A.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference79 articles.

1. Oscillatory zoning: a pathological case of crystal growth;Allègre;Nature,1981

2. Local equilibrium of mafic enclaves and granitoids of the Turtle pluton, southeast California: Mineral, chemical and isotopic evidence;Allen;Am. Mineral.,1991

3. Appinites, lamprophyres and mafic micro-granular enclaves: Three related products of interaction between acid and basic magmas;Ayrton,1991

4. Tracer versus trace element diffusion: Diffusional decoupling of Sr concentration from Sr isotopic composition;Baker;Geochim. Cosmochim. Acta,1989

5. Granite and granodiorite at Powelltown, Victoria, and their relationships;Baker,1938

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