Physics
Scientific paper
Sep 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001e%26psl.192...57h&link_type=abstract
Earth and Planetary Science Letters, Volume 192, Issue 1, p. 57-63.
Physics
2
Scientific paper
Exhumation of subducted continental crust to the Earth's surface was presumably rapid, though at an uncertain rate, to retain coesite, diamond and α-PbO2-type TiO2. Here we report unique defect microstructures of minerals as a potential indicator of a rapid and episodic exhumation process in a fossil fracture zone of coesite eclogite from the Sulu terrain, eastern China having the most negative δ18O value ever reported for eclogite-facies metamorphic rock. Analytical electron microscopy indicates that semi-brittle deformation occurred in kyanite/omphacite/spinel with extensive and unusual fine-scale twin lamellae and that brittle deformation occurred in garnet with hardly healed {110} microcleavages. These unique defect microstructures can be rationalized by a high strain rate at local weakening and deep faulting of continental collision orogens.
Chu Hao-Tsu
Hwang Shyh-Lung
Shen Peiruo
Yui Tzen-Fu
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