메뉴 건너뛰기




Volumn 27, Issue 5-6, 1998, Pages 631-645

The origin of hypersaline liquid in the quaternary Kakkonda granite, sampled from well WD-1a, Kakkonda geothermal system, Japan

Author keywords

Fluid inclusion; Geochemistry; Geothermal model; Isotope; Japan; Kakkonda; PTX analysis; Salinity

Indexed keywords

EXPLORATORY GEOCHEMISTRY; GEOTHERMAL WELLS; GRANITE; PHASE SEPARATION; SODIUM CHLORIDE; THERMAL STRESS; TRITIUM; WELL DRILLING;

EID: 0345148804     PISSN: 03756505     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0375-6505(98)00037-6     Document Type: Article
Times cited : (35)

References (26)
  • 2
    • 0001521883 scopus 로고
    • Fluid-inclusion evidence for a magmatic source for metals in porphyry copper deposits
    • ed. J. F. H. Thompson Mineral. Assoc. Can., Short Course
    • Bodnar, R. J. (1995) Fluid-inclusion evidence for a magmatic source for metals in porphyry copper deposits. In Magmas, Fluids, and Ore Deposits, ed. J. F. H. Thompson, Vol. 23, pp. 139-152. Mineral. Assoc. Can., Short Course.
    • (1995) In Magmas, Fluids, and Ore Deposits , vol.23 , pp. 139-152
    • Bodnar, R.J.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.