| DOI: | 10.1306/02171514097
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| Scopus记录号: | 2-s2.0-84938795768
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| 论文题名: | Diagenetic barite and sphalerite in middle Mesozoic sandstones, Scotian Basin, as tracers for basin hydrology |
| 作者: | Pe-Piper G.; Piper D.J.W.; Zhang Y.; Chavez I.
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| 刊名: | AAPG Bulletin
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| ISSN: | 0149-1508
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| EISSN: | 1558-9238
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| 出版年: | 2015
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| 发表日期: | 2015
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| 卷: | 99, 期:7 | | 起始页码: | 1281
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| 结束页码: | 1313
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| 语种: | 英语
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| Scopus关键词: | Barite
; Cementing (shafts)
; Faulting
; Flow of fluids
; Isotopes
; Kaolinite
; Manganese
; Minerals
; Saline water
; Salt tectonics
; Sandstone
; Scanning electron microscopy
; Seismology
; Tectonics
; Titanium oxides
; Zinc sulfide
; Carbonate cementation
; Detachment fault
; Electron microprobes
; Long-distance transport
; Saline formation
; Secondary porosity
; Seismic interpretation
; Tectonic evolution
; Transport properties
; barite
; basin analysis
; cementation
; detachment fault
; evaporite
; fluid flow
; geochemistry
; hydrocarbon
; hydrology
; isotopic analysis
; Mesozoic
; porosity
; sandstone
; scanning electron microscopy
; seismic data
; sphalerite
; tectonic evolution
; Canada
; Nova Scotia
|
| Scopus学科分类: | Energy
; Earth and Planetary Sciences
|
| 英文摘要: | Cementation of sandstone by minor late barite and sphalerite is widespread in the Scotian Basin at burial depths >2 km (>1 mi), providing information on fluid flow in the basin. The texture and geochemistry of these minerals were analyzed by scanning electron microscopy and electron microprobe on samples from conventional core. Barite and sphalerite postdate silica and carbonate cementation, occurring in veins or occupying secondary porosity. They occur with diagenetic chlorite, kaolinite, pyrite, titania minerals, kutnohorite, and Mn-siderite. This study relates barite and sphalerite to the salt-tectonic evolution of the basin, based on seismic interpretation, and the thermal history of the basin, based on fluid inclusion studies. Barite is readily transported in basinal fluids >100°C (212°F), yet is consistently a very late diagenetic mineral. This implies that the source of Ba is because of the late diagenetic breakdown of K-feldspars at 2-3 km (1-2 mi) depth, which is confirmed by covariation of Ba and Rb in sandstones. Sulfur isotope data suggest that the SO4 2+ was derived from Argo Formation evaporites that include 1%-7% anhydrite. Sphalerite is mobile only in saline formation water >140°C (°284°F) and requires long-distance transport through sandstones with Zn-rich Fe-Ti oxides. Active detachment faults on salt welds provide potential pathways and a source of salt for migrating formation water. The particularities of source and transport of both barite and sphalerite allow the pathways of basinal fluids and their relationship to active salt tectonics to be inferred, providing indirect dating of the later stages of diagenetic pangenesis corresponding to times of hydrocarbon charge. Copyright ©. The American Association of Petroleum Geologists. All rights reserved. |
| URL: | https://www.scopus.com/inward/record.uri?eid=2-s2.0-84938795768&doi=10.1306%2f02171514097&partnerID=40&md5=d8c4204ef9626a45cdde8e07364080db
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| Citation statistics: |
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| 资源类型: | 期刊论文
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| 标识符: | http://119.78.100.158/handle/2HF3EXSE/13079
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| Appears in Collections: | 过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响
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| Recommended Citation: | |
Pe-Piper G.,Piper D.J.W.,Zhang Y.,et al. Diagenetic barite and sphalerite in middle Mesozoic sandstones, Scotian Basin, as tracers for basin hydrology[J]. AAPG Bulletin,2015-01-01,99(7)
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