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Shock-induced high-pressure phase transition of labradorite to hollandite "(Na-47-Ca-51-K-2)" in Zagami and the assemblage hollandite "(Na-80-Ca-12-K-8)" plus jadeite in L chondrites: Constraints to peak shock pressures.
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
2000 (English)In: METEORITICS & PLANETARY SCIENCE, Vol. 35, A51-A51 p.Other (Other scientific)
Place, publisher, year, pages
METEORITICAL SOC , 2000. Vol. 35, A51-A51 p.
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URN: urn:nbn:se:uu:diva-37703OAI: oai:DiVA.org:uu-37703DiVA: diva2:65602
Note
Addresses: Max Planck Inst Chem, D-55128 Mainz, Germany. Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China. Ecole Normale Super Lyon, F-69364 Lyon, France. Uppsala Univ, Inst Earth Sci, S-75236 Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17

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