RELEASE OF TRACE ELEMENTS THROUGH THE SUB-GREENSCHIST FACIES BREAKDOWN OF DETRITAL RUTILE TO METAMORPHIC TITANITE IN THE OTAGO SCHIST, NEW ZEALAND-Reference-Cited by-同舟云学术

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RELEASE OF TRACE ELEMENTS THROUGH THE SUB-GREENSCHIST FACIES BREAKDOWN OF DETRITAL RUTILE TO METAMORPHIC TITANITE IN THE OTAGO SCHIST, NEW ZEALAND

Published:2015-05 Issue:3 Volume:53 Page:379-400
ISSN:0008-4476
Container-title:The Canadian Mineralogist
language:en
Short-container-title:Can Mineral

Author:

Cave Ben J.,Stepanov Aleksandr S.,Craw Dave,Large Ross R.,Halpin Jacqueline A.,Thompson Jay

Publisher

Mineralogical Association of Canada

Subject

Geochemistry and Petrology

Cited by 28 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. Geochemistry of metasedimentary restitic rocks and implications for melting conditions and metal potential of crustal felsic magmas;Earth-Science Reviews;2024-07

2. Navigating the complexity of detrital rutile provenance: methodological insights from the Neotethys Orogen in Anatolia;Geochronology;2024-06-17

3. Predictive Models for Detrital Titanite Provenance With Application to the Nanga Parbat—Haramosh Syntaxial Massif, Western Himalaya;Journal of Geophysical Research: Earth Surface;2024-04-29

4. Compositional changes in garnet: trace element transfer during eclogite-facies metamorphism;Contributions to Mineralogy and Petrology;2023-09-11

5. Detrital Garnet Geochronology by In Situ U‐Pb and Lu‐Hf Analysis: A Case Study From the European Alps;Journal of Geophysical Research: Earth Surface;2023-09

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