@article{752027,
      author = {Xie, Xiande, and Chen, Ming},
      url = {http://library.usi.edu/record/752027},
      title = {Suizhou meteorite mineralogy and shock metamorphism /  [electronic resource] :},
      abstract = {This book introduces the unusual shock-related  mineralogical features of the shocked Suizhou L6 (S5)  meteorite. The olivine and pyroxene in Suizhou display a  mosaic shock feature, while most of plagioclase grains have  transformed to glassy maskelynite. A few of the  shock-induced melt veins in the meteorite are the simplest,  straightest and thinnest ones among all shock-vein-bearing  meteorites, and contain the most abundant high-pressure  mineral species. Among the 11 identified species, tuite,  xieite, and the post-spinel CF-phase of chromite are new  minerals. The meteorite experienced a peak shock pressure  up to 24 GPa and temperatures of up to 1000° C. Locally  developed shock veins were formed at the same pressure, but  at an elevated temperature of about 2000° C that was  produced by localized shear-friction stress. The rapid  cooling of the extremely thin shock veins is the main  reason why 11 shock-induced high-pressure mineral phases  could be preserved in them so well. This book offers a  helpful guide for meteoritics researchers and mineralogists  and invaluable resource for specialists working in  high-pressure and high-temperature mineralophysics.},
      doi = {https://doi.org/10.1007/978-3-662-48479-1},
      recid = {752027},
      pages = {1 online resource.},
}