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DOI | 10.1306/02151918034 |
Fluid-flow evolution in the Albanide fold-thrust belt: Insights from hydrogen and oxygen isotope ratios of fluid inclusions | |
de Graaf, Stefan1,2,3; Nooitgedacht, Casimir W.4,5; Le Goff, Johan5; van der Lubbe, Jeroen H. J. L.4; Vonhof, Hubert B.6; Reijmer, John J. G.5 | |
2019-10-01 | |
发表期刊 | AAPG BULLETIN |
ISSN | 0149-1423 |
EISSN | 1558-9153 |
出版年 | 2019 |
卷号 | 103期号:10页码:2421-2445 |
文章类型 | Article |
语种 | 英语 |
国家 | Saudi Arabia; Netherlands; Germany |
英文摘要 | Tectonic forces generated during thrust emplacement along active margins may drive complex fluid-flow patterns in fold-thrust belts and foreland basins. Isotope data (delta(2)Hand delta O-18) of fluid inclusions hosted in calcite vein cements are used to reconstruct regional fluid migration pathways in the Albanide fold-thrust system. The calcite veins used in this study developed in a sequence of naturally fractured Cretaceous-Eocene carbonate rocks as a result of episodic throughput of fluids from the early stages of burial onward. The acquired fluid inclusion isotope data demonstrate that fluids circulating in the carbonates were derived from an underlying reservoir that consisted of a mixture of meteoric water and evolved marine fluids, probably derived from deep-seated evaporites. The meteoric fluids infiltrated in the hinterland before being driven outward into the foreland basin and ascended as soon as fracturing induced a sufficient increase in permeability. Structural and petrographic observations provide time constraints for the various phases of fracture infilling and reveal an increasing dominance of meteoric water in the system through time as migration pathways shortened and marine formation fluids were progressively flushed out. Similar fluid-flow evolutions have previously been recorded in various fold-thrust belt settings elsewhere in the world. |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000489899900007 |
WOS关键词 | FORELAND BASIN ; IONIAN-BASIN ; CARBONATE RESERVOIR ; FLEXURAL EXTENSION ; TECTONIC EVOLUTION ; JANDAIRA FORMATION ; DELTA-O-18 VALUES ; PALEOFLUID-FLOW ; GEOLOGICAL TIME ; GROWTH-RATE |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/187162 |
专题 | 地球科学 |
作者单位 | 1.King Fahd Univ Petr & Minerals, Coll Petr Engn & Geosci CPG, Dhahran, Saudi Arabia; 2.Vrije Univ VU Amsterdam, Fac Sci, Dept Earth Sci, Amsterdam, Netherlands; 3.Max Planck Inst Chem, Dept Climate Geochem, Mainz, Germany; 4.Vrije Univ Amsterdam, Dept Earth Sci, Fac Sci, Amsterdam, Netherlands; 5.KFUPM, CPG, Dhahran, Saudi Arabia; 6.MPIC, Dept Climate Geochem, Mainz, Germany |
推荐引用方式 GB/T 7714 | de Graaf, Stefan,Nooitgedacht, Casimir W.,Le Goff, Johan,et al. Fluid-flow evolution in the Albanide fold-thrust belt: Insights from hydrogen and oxygen isotope ratios of fluid inclusions[J]. AAPG BULLETIN,2019,103(10):2421-2445. |
APA | de Graaf, Stefan,Nooitgedacht, Casimir W.,Le Goff, Johan,van der Lubbe, Jeroen H. J. L.,Vonhof, Hubert B.,&Reijmer, John J. G..(2019).Fluid-flow evolution in the Albanide fold-thrust belt: Insights from hydrogen and oxygen isotope ratios of fluid inclusions.AAPG BULLETIN,103(10),2421-2445. |
MLA | de Graaf, Stefan,et al."Fluid-flow evolution in the Albanide fold-thrust belt: Insights from hydrogen and oxygen isotope ratios of fluid inclusions".AAPG BULLETIN 103.10(2019):2421-2445. |
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