Regional fluid charecters and regimes of "Sanjiang" middle belt during Neo-Tethys

Acta Petrologica Sinica

Volumn 16, Issue 4, 2000, Pages 639-648

  Qidong, X ^a   Xuanxue, M ^a  

^a CHINA UNIVERSITY OF GEOSCIENCES   (China)

Author keywords

Fluid inclusion; Fluid regime; Polymetallic mineralization; Stable isotope; Tethys

Indexed keywords

CARBON DIOXIDE; GEOLOGY; ISOTOPES; MINERALOGY; TEMPERATURE;

FLUID INCLUSION; FLUID REGIME; POLYMETALLIC; STABLE ISOTOPES; TETHYS;

FLOW OF FLUIDS;

FLUID DYNAMICS; FLUID INCLUSION; HYDROTHERMAL FLUID; MINERALIZATION; TETHYS;

CHINA;

EID: 84978012308     PISSN: 10000569     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (21)

1. Silver-lead-zinc vein, metamorphic core complexes, and hydrologic regimes during crustal extension
2. Stable isotopic and fluid inclusion evidence for meteoric fluid penetration into an active mountain belt, Alpine Schist, New Zealand
3. Fluid regimes during late stages of a continental collision: Physical, chemical, and sable isotope measurements of fluid inclusions in fissure quartz from a geotraverse through the Central Alps
4. Geochemical studies of the origins and effects of synorogenic crustal fluids in the Southern Omineca Belt of British Columbia, Canada
5. Paleo-hydrogeology of late Proterozoic units of Southeastern Canadian Cordillera
6. Fortran programs for calculation of fluid properties from microthermometric data on fluid inclusions
7. 2O
8. The relations between mean rock stress and fluid flow in the crust: With reference to vein- and lode-style gold deposits
9. The theoretical schema and methods for the geochemical study of metallogenic province and belts