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Multistage hydrothermal dolomites in the Middle Devonian (Givetian) carbonates from the Guilin area, South China

文献类型:期刊论文

作者Chen, DZ; Qing, HR; Yang, C
刊名SEDIMENTOLOGY
出版日期2004-10-01
卷号51期号:5页码:1029-1051
关键词China Devonian diagenesis dolomitization hydrothermal fluids
ISSN号0037-0746
DOI10.1111/j.1365-3091.2004.00659.x
文献子类Article
英文摘要Pervasive dolomites occur preferentially in the stromatoporoid biostromal (or reefal) facies in the basal Devonian (Givetian) carbonate rocks in the Guilin area, South China. The amount of dolomites, however, decreases sharply in the overlying Frasnian carbonate rocks. Dolostones are dominated by replacement dolomites with minor dolomite cements. Replacement dolomites include: (1) fine to medium, planar-e floating dolomite rhombs (Rd1); (2) medium to coarse, planar-s patchy/mosaic dolomites (Rd2); and (3) medium to very coarse non-planar anhedral mosaic dolomites (Rd3). They post-date early submarine cements and overlap with stylolites. Two types of dolomite cements were identified: planar coarse euhedral dolomite cements (Cd1) and non-planar (saddle) dolomite cements (Cd2); they post-date replacement dolomites and predate late-stage calcite cements that line mouldic vugs and fractures. The replacement dolomites have delta(18)O values from -13.7 to -9.7% VPDB, delta(13)C values from -2.7 to + 1.5% VPDB and Sr-87/Sr-86 ratios from 0.7082 to 0.7114. Fluid inclusion data of Rd3 dolomites yield homogenization temperatures (T-h) of 136-149degreesC and salinities of 7.2-11.2 wt% NaCl equivalent. These data suggest that the replacive dolomitization could have occurred from slightly modified sea water and/or saline basinal fluids at relatively high temperatures, probably related to hydrothermal activities during the latest Givetian-middle Fammenian and Early Carboniferous times. Compared with replacement dolomites, Cd2 cements yield lower delta(18)O values (-14.2 to -9.3% VPDB), lower delta(13)C values (-3.0 to -0.7% VPDB), higher Sr-87/Sr-86 ratios (approximate to0.7100) and higher T-h values (171-209degreesC), which correspond to trapping temperatures (T-r) between 260 and 300degreesC after pressure corrections. These data suggest that the dolomite cements precipitated from higher temperature hydrothermal fluids, derived from underlying siliciclastic deposits, and were associated with more intense hydrothermal events during Permian-Early Triassic time, when the host dolostones were deeply buried. The petrographic similarities between some replacement dolomites and Cd2 dolomite cements and the partial overlap in Sr-87/Sr-86 and delta(18)O values suggest neomorphism of early formed replacement dolomites that were exposed to later dolomitizing fluids. However, the dolomitization was finally stopped through invasion of meteoric water as a result of basin uplift induced by the Indosinian Orogeny from the early Middle Triassic, as indicated by the decrease in salinities in the dolomite cements in veins (5.1-0.4 wt% NaCl equivalent). Calcite cements generally yield the lowest delta(18)O values (-18.5 to -14.3% VPDB), variable delta(13)C values (-11.3 to -1.2% VPDB) and high T-h values (145-170degreesC) and low salinities (0-0.2 wt% NaCl equivalent), indicating an origin of high-temperature, dilute fluids recharged by meteoric water in the course of basin uplift during the Indosinian Orogeny. Faults were probably important conduits that channelled dolomitizing fluids from the deeply buried siliciclastic sediments into the basal carbonates, leading to intense dolomitization (i.e. Rd3, Cd1 and Cd2).
WOS关键词CANADA SEDIMENTARY BASIN ; MEADOWBROOK REEF TREND ; WEST-CENTRAL ALBERTA ; FLUID-FLOW ; PRESQUILE BARRIER ; DOLOMITIZATION ; ORIGIN ; HILLS ; FIELD ; FAULT
WOS研究方向Geology
语种英语
WOS记录号WOS:000224024800006
出版者BLACKWELL PUBLISHING LTD
源URL[http://ir.iggcas.ac.cn/handle/132A11/64271]  
专题中国科学院地质与地球物理研究所
通讯作者Chen, DZ
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Univ Regina, Dept Geol, Regina, SK S4S 0A2, Canada
推荐引用方式
GB/T 7714
Chen, DZ,Qing, HR,Yang, C. Multistage hydrothermal dolomites in the Middle Devonian (Givetian) carbonates from the Guilin area, South China[J]. SEDIMENTOLOGY,2004,51(5):1029-1051.
APA Chen, DZ,Qing, HR,&Yang, C.(2004).Multistage hydrothermal dolomites in the Middle Devonian (Givetian) carbonates from the Guilin area, South China.SEDIMENTOLOGY,51(5),1029-1051.
MLA Chen, DZ,et al."Multistage hydrothermal dolomites in the Middle Devonian (Givetian) carbonates from the Guilin area, South China".SEDIMENTOLOGY 51.5(2004):1029-1051.

入库方式: OAI收割

来源:地质与地球物理研究所

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