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Volumn 41, Issue 9, 2000, Pages 1455-1466

Two disequilibrium quartz-feldspar 18O/16O fractionations within the Aral granite batholith, Altay Mountains of China: Evidence for occurrence of two stages of O and H isotopic exchange of a heterogeneous granite system with aqueous fluids

Author keywords

Altay; Granite; Initial 18O 16O heterogeneity; Pseudoisotherm; Quartz feldspar 18O 16O reversal

Indexed keywords

BATHOLITH; DEUTERIUM; FELDSPAR; GRANITE; HYDROGEN; OXYGEN ISOTOPE; QUARTZ; WATER-ROCK INTERACTION;

EID: 0033827446     PISSN: 00223530     EISSN: None     Source Type: Journal    
DOI: 10.1093/petrology/41.9.1455     Document Type: Article
Times cited : (16)

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  • 20
    • 0030738605 scopus 로고    scopus 로고
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  • 37


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.