Back-transformation of high-pressure phases in a shock melt vein of an H-chondrite during atmospheric passage: Implications for the survival of high-pressure phases after decompression
- 1 January 2004
- journal article
- Published by Elsevier BV in Earth and Planetary Science Letters
- Vol. 217 (1-2), 141-150
- https://doi.org/10.1016/s0012-821x(03)00585-5
Abstract
No abstract availableKeywords
Funding Information
- Chinese Academy of Sciences (KJCX2-SW-NO3, KZCX3-SW-123)
- Ministry of Education, Culture, Sports, Science and Technology (09640562, 11640473)
This publication has 17 references indexed in Scilit:
- Metal-troilite-magnetite assemblage in shock veins of Sixiangkou meteoriteGeochimica et Cosmochimica Acta, 2002
- A comparative study of naturally and experimentally shocked chondritesEarth and Planetary Science Letters, 2001
- Anatomy of black veins in Zagami: clues to the formation of high-pressure phasesEarth and Planetary Science Letters, 2000
- Natural NaAlSi 3 O 8 -Hollandite in the Shocked Sixiangkou MeteoriteScience, 2000
- The fusion crusts of stony meteorites: Implications for the atmospheric reprocessing of extraterrestrial materialsMeteoritics & Planetary Science, 1999
- Natural Occurrence of MgSiO 3 -Ilmenite and Evidence for MgSiO 3 -Perovskite in a Shocked L ChondriteScience, 1997
- The Majorite-Pyrope + Magnesiowüstite Assemblage: Constraints on the History of Shock Veins in ChondritesScience, 1996
- Melting experiments on anhydrous peridotite KLB‐1 from 5.0 to 22.5 GPaJournal of Geophysical Research, 1994
- Shock metamorphism of ordinary chondritesGeochimica et Cosmochimica Acta, 1991
- Thermal expansion of modified spinel, .BETA.-Mg2SiO4.Journal of Physics of the Earth, 1980