The distinct morphological and petrological features of shock melt veins in the Suizhou L6 chondrite

• Published in: Meteoritics & planetary science Vol. 46; no. 3; pp. 459 - 469
• Main Authors: XIE, Xiande, SUN, Zhenya, CHEN, Ming
• Format: Journal Article
• Language: English
• Published: Oxford, UK Blackwell Publishing Ltd 01.03.2011; Wiley Subscription Services, Inc
• Subjects: Chondrites; Melts; Meteorites; Minerals; Phases; Plagioclase; Scanning electron microscopy; Veins
• ISSN: 1086-9379; 1945-5100
• DOI: 10.1111/j.1945-5100.2011.01168.x

– The morphology and petrology of distinct melt veins in the Suizhou L6 chondrite have been investigated using scanning electron microscopy, electron microprobe analyses, and Raman spectroscopy, synchrotron energy‐dispersive diffraction, and transmission electron microscopy. It is found that the melt veins in the Suizhou meteorite morphologically are the simplest, straightest, and thinnest among all shock veins known from meteorites. At first glance, these veins look like fine fractures, but petrologically they are solid melt veins of chondritic composition and consist of fully crystalline materials of two distinct lithological assemblages, with no glassy material remaining. The Suizhou melt veins contain the most abundant high‐pressure mineral species when compared with all other veins known in chondrites. Thus, these veins in Suizhou are classified as shock veins. All rock‐forming and almost all accessory minerals in the Suizhou shock veins have been transformed to their high‐pressure polymorphs, and no fragments of the precursor minerals remain in the veins. Among the 11 high‐pressure mineral phases identified in the Suizhou veins, three are new high‐pressure minerals, namely, tuite after whitlockite, xieite, and the CF phase after chromite. On the basis of transformation of plagioclase into maskelynite, it is estimated that the Suizhou meteorite experienced shock pressures and shock temperatures up to 22 GPa and 1000 °C, respectively. Shearing and friction along shock veins raised the temperature up to 1900–2000 °C and the pressure up to 24 GPa within the veins. Hence, phase transition and crystallization of high‐pressure minerals took place only in the Suizhou shock veins. Fast cooling of the extremely thin shock veins is regarded as the main reason that up to 11 shock‐induced high‐pressure mineral phases could be preserved in these veins.