Incipient devitrification of impact melt particles at Bosumtwi crater, Ghana: Implications for suevite cooling history and melt dispersion-Reference-Cited by-同舟云学术

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Incipient devitrification of impact melt particles at Bosumtwi crater, Ghana: Implications for suevite cooling history and melt dispersion

Published:2018-12-11 Issue:10 Volume:54 Page:2557-2572
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Välja Rudolf¹,Kirsimäe Kalle¹^ORCID,Koeberl Christian²³^ORCID,Boamah Daniel⁴,Kirs Juho¹

Affiliation:

1. Department of Geology University of Tartu Ravila 14A 50411 Tartu Estonia

2. Department of Lithospheric Research University of Vienna Althanstrasse 14 1090 Vienna Austria

3. Natural History Museum Burgring 7 1010 Vienna Austria

4. Ghana Geological Survey Department P.O. Box M80 Accra Ghana

Funder

Eesti Teadusagentuur

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.13225

Reference64 articles.

1. Geochemistry, genesis, and health implications of fluoriferous groundwaters in the upper regions of Ghana

2. Possible reasons of shock melt deficiency in the Bosumtwi drill cores

3. Investigating the Lake Bosumtwi impact structure: Insight from numerical modeling

4. Ries crater and suevite revisited-Observations and modeling Part II: Modeling

5. Plagioclase nucleation and growth kinetics in a hydrous basaltic melt by decompression experiments

Cited by 3 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. The Luna structure, India: A probable impact crater formed by an iron bolide;Planetary and Space Science;2024-01

2. Microporphyritic and microspherulitic melt grains, Hiawatha crater, Northwest Greenland: Implications for post-impact cooling rates, hydration, and the cratering environment;GSA Bulletin;2022-01-05

3. Microporphyritic and microspherulitic melt grains, Hiawatha crater, Northwest Greenland: Implications for post-impact cooling rates, hydration, and the cratering environment;GEOL SOC AM BULL;2022

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