Petrological structure and thermal structure of the Dabie orogenic belt and its geological implications

Acta Geologica Sinica (English Edition)

Volumn 74, Issue 3, 2000, Pages 206-215

  Deng, J ^a   Dai, S ^a   Wu, Z ^a   Zhao, H ^a   Du, J ^a   Luo, Z ^a  

^a CHINA UNIVERSITY OF GEOSCIENCES   (China)

Author keywords

Dabie orogenic belt; Orogenic deep processes; Petrological structure; Thermal structure; UHP rook

Indexed keywords

OROGENIC BELT; PETROLOGY; TECTONIC EVOLUTION; THERMAL STRUCTURE;

CHINA; DABIE SHAN;

EID: 0033792994     PISSN: 10009515     EISSN: 17556724     Source Type: Journal    
DOI: None     Document Type: Article

References (26)

1. Garnet-omphacite-phengite barometry of eclogites in Dabieshan, Central China
2. Coesite-bearing eclogites from the Bixiling Complex, Dabie nountains, China: Sm-Nd ages, geochemical characteristics and tectonic implications
3. Some thermal and tectonic models for crustal melting in continental collision zones
4. P-and S-wave velocities and densities of rocks from the Dabie ultrahigh-pressure (UHP) metamorphic belt to pressure of 600 MPa and to temperature of 600°C
5. Ultra high-P metamorphic rocks and their associated lithologies from the Dabie mountain, Central China: A field trip guide to the 3rd International Eclogite Field Symposium
6. Seeing a mountain in a grain of garnet
7. Melting of vapour-absent tonalile at 10 kbar to simnlate dehydration-melting in the deep crust
8. Petrographic evidences for the uplift of eclofite in the Dabie mountain, China
9. Ultrahigh-pressure metamorphiom of the Sulu Terrance, Eastern China: A prospction view Contin.