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- W303609639 abstract "Recent highway construction across the Qinglong Mountains in Donghai, eastern China (Figure 1) has exposed a 660 m section of gneiss, eclogite, and minor quartzite. The outcrop consists of steeply SE-dipping layers cut by several high-angle (normal?) faults (Figure 2). Eclogite layers are concordant with gneissic rocks and minor quartzites; a few discordant eclogite contacts (e.g., QL16) appear to be intrusive. Most eclogites are characterized by abundant hydrous phases including talc, phengite, and epidote; many also contain kyanite. The Qinglong Mountains contain a variety of UHP eclogites, and are the classic locality for negative δ18O values (-14 to -16‰) for UHP minerals in eclogites, quartzites and surrounding gneisses (Yui et al. 1994; Rumble and Yui 1998) indicating that fluid may have been absent during metamorphism. Inclusions of coesite and coesite pseudomorphs in UHP phases, including epidote and kyanite from both eclogite and quartzite, of this region were reported by Zhang et al. (1995; in review). This region lies about 22 km NE from the Chinese Continental Scientific Drilling site in Donghai. Therefore, petrotectonic information derived from this continuous exposure of eclogitic and gneissic rocks is applicable to the CCSD site." @default.
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- W303609639 date "2001-12-01" @default.
- W303609639 modified "2023-09-26" @default.
- W303609639 title "P-T ESTIMATES FOR PHENGITE-KYANITE UHP ECLOGITES FROM A HIGHWAY ROADCUT NEAR THE QINGLONG MOUNTAINS, EASTERN CHINA" @default.
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