Enigmatic textures developed along plagioclase-augite grain boundaries at the base of the Main Zone, Northern Limb, Bushveld Complex - evidence for late stage melt infiltration into a nearly solidified crystal mush-Reference-Cited by-同舟云学术

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Enigmatic textures developed along plagioclase-augite grain boundaries at the base of the Main Zone, Northern Limb, Bushveld Complex - evidence for late stage melt infiltration into a nearly solidified crystal mush

Published:2009-03-01 Issue:1 Volume:112 Page:39-46
ISSN:1012-0750
Container-title:South African Journal of Geology
language:en
Short-container-title:South African Journal of Geology

Author:

Roelofse F.,Ashwal L.D.,Pineda-Vargas C.A.,Przybylowicz W.J.

Publisher

Geological Society of South Africa

Subject

Geology

Cited by 10 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. Formation of Spinel-Orthopyroxene Symplectites by Reactive Melt Flow: Examples from the Northern Bushveld Complex and Implications for Mineralization in Layered Intrusions;Economic Geology;2022-12-01

2. Microstructures and Late-Stage Magmatic Processes in Layered Mafic Intrusions: Symplectites from the Sept Iles Intrusion, Quebec, Canada;Journal of Petrology;2020-07-01

3. The Merensky Cyclic Unit, Bushveld Complex, South Africa: Reality or Myth?;Minerals;2018-04-03

4. Interstitial microstructures in Ji'nan mafic intrusion, North China Craton: magmatic or hydrothermal origin?;European Journal of Mineralogy;2017-12-15

5. Large-scale magmatic layering in the Main Zone of the Bushveld Complex and episodic downward magma infiltration;Contributions to Mineralogy and Petrology;2017-02-25

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