Discovery of eclogite inclusions and its geological significance in early Jurassic intrusive complex in Xuzhounorthern Anhui, eastern China

التفاصيل البيبلوغرافية
العنوان: Discovery of eclogite inclusions and its geological significance in early Jurassic intrusive complex in Xuzhounorthern Anhui, eastern China
المؤلفون: Qing-Hai Wang, Wen-Liang Xu, Jingqian Lin, Xiaochun Liu, Dongyan Wang
المصدر: Chinese Science Bulletin. 47:1212-1216
بيانات النشر: Springer Science and Business Media LLC, 2002.
سنة النشر: 2002
مصطلحات موضوعية: Multidisciplinary, biology, Metamorphic rock, Geochemistry, Metamorphism, engineering.material, biology.organism_classification, Almandine, Augite, engineering, Xenolith, Omphacite, Eclogite, Petrology, Geology, Metamorphic facies
الوصف: The early Jurassic intrusive complex is chiefly made of monzodioritic porphyry in northern Anhui and northern Jiangsu, which emplaced in 191 Ma. The intrusive complexes contain a lot of eclogite inclusions which belong to eclogite and garnet-pyroxenite. The inclusions had undergone eclogite facies high-pressure metamorphism and amphibolite facies retrogressive metamorphism. The garnets in eclogite inclusions are mainly almandine varieties and clinopyroxenes are omphacite and augite. The mineral assemblage andP-T estimation results show thatP-T conditions of eclogite facies metamorphism and amphibolite facies retrogressive metamorphism are over 1.2–1.5 GPa, 709–861°C and 0.7–1.03 GPa, 666–738°C, respectively. The discovery of the high-pressure xenoliths not only is of important significance to understand the composition and structure of deep crust in southern edge of North China Platform, but also can be of important influence on realizing the subduction-collision-exhumation evolutional process of the Dabie-Sulu ultrahigh-pressure (UHP) metamorphic belt.
تدمد: 1861-9541
1001-6538
DOI: 10.1007/bf02907612
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_________::1960aabdf4c695ce41cd008100448f18
https://doi.org/10.1007/bf02907612
Rights: CLOSED
رقم الانضمام: edsair.doi...........1960aabdf4c695ce41cd008100448f18
قاعدة البيانات: OpenAIRE
الوصف
تدمد:18619541
10016538
DOI:10.1007/bf02907612