Porphyry mo and greisen w metallogeny related to the karamea batholith, south island, new zealand (note)

4Citations
Citations of this article
6Readers
Mendeley users who have this article in their library.

Abstract

Porphyry Mo and greisen W deposits in west Nelson-Westland, New Zealand, are associated with the Tuhuan (Lower Paleozoic) phase and Rangitata (Cretaceous) phase respectively of the Karamea Batholith. Porphyry Mo deposits are locally spatially associated with various rocks of the Western Sedimentary Belt, whereas greisen W deposits are found exclusively with Greenland Group rocks and genetically associated with high-level greisenised stocks. In the latter deposits, scheelite is the chief ore mineral. The salient geological features of these deposits are briefly outlined. Metallogenesis reflects a collision-dominated tectonic regime for W and a subduction environment for Mo. © 1985 Taylor & Francis Group, LLC.

Cite

CITATION STYLE

APA

Pirajno, F. (1985). Porphyry mo and greisen w metallogeny related to the karamea batholith, south island, new zealand (note). New Zealand Journal of Geology and Geophysics, 28(1), 187–191. https://doi.org/10.1080/00288306.1985.10422283

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free