Model for the development of kyanite during partial convective overturn of Archean granite–greenstone terranes: the Pilbara Craton, Australia
Author:
Affiliation:
1. Department of Geology, University of Newcastle, Newcastle, NSW 2308, Australia
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1525-1314.1999.00187.x
Cited by 57 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. Comment on “Subsurface distribution of granites and greenstones in the paleoarchean east Pilbara terrane from 3-D gravity inversion”;Precambrian Research;2024-09
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3. Constraints on the age of dome-and-keel structures in the Pilbara Craton through integrated garnet geochronology and microstructural analyses;Precambrian Research;2023-08
4. Spatial and temporal control of Archean tectonomagmatic regimes;Earth-Science Reviews;2023-06
5. Vertical tectonics of a Neoarchean gneiss dome in the eastern North China Craton;Geological Journal;2023-05-14
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