二叠纪分水岭钨矿床（澳大利亚昆士兰州东北部）：流体包裹体和稳定同位素制约因素

IF 1.2 4区地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY

Australian Journal of Earth Sciences Pub Date : 2024-09-01 DOI:10.1080/08120099.2024.2390686

J. A. Poblete, J-M. Huizenga, Z. Chang, P. Dirks

引用次数: 0

摘要

分水岭白钨矿床位于昆士兰州北部莫斯曼造山带一个已消亡的前弧盆地中。该前弧地区由奥陶纪-志留纪多变形的玄武岩组成。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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The Permian Watershed tungsten deposit (northeast Queensland, Australia): fluid inclusion and stable isotope constraints

The Watershed scheelite deposit is located in an extinct fore-arc basin in the Mossman Orogen of North Queensland. This fore-arc region comprises multiply deformed, Ordovician–Silurian metasediment...

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来源期刊

Australian Journal of Earth Sciences 地学-地球科学综合

CiteScore

2.80

自引率

8.30%

发文量

审稿时长

6-12 weeks

期刊介绍： Australian Journal of Earth Sciences publishes peer-reviewed research papers as well as significant review articles of general interest to geoscientists. The Journal covers the whole field of earth science including basin studies, regional geophysical studies and metallogeny. There is usually a thematic issue each year featuring a selection of papers on a particular area of earth science. Shorter papers are encouraged and are given priority in publication. Critical discussion of recently published papers is also encouraged.