气候变化领域集成服务门户(CCPortal): Depositional controls on sediment properties in dryland rivers: Influence on near-surface diagenesis

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DOI	10.1016/j.earscirev.2020.103297
	Depositional controls on sediment properties in dryland rivers: Influence on near-surface diagenesis
	Henares S.; Donselaar M.E.; Caracciolo L.
发表日期	2020
ISSN	00128252
卷号	208
英文摘要	Sandy braided dryland rivers, deposited under arid to semi-arid conditions, constitute important clastic reservoirs worldwide whose reservoir quality reflects the effect of primary sediment properties on near-surface diagenetic processes. A literature review is presented of existing facies models, based on geomorphological analysis of modern perennial braided rivers, further illustrated with own outcrop and subsurface examples of dryland river deposits in: (a) Argana Basin (Triassic, Morocco), (b) Iberian Meseta (Triassic, Central SE Spain), (c) Huesca Fluvial Fan (Miocene, Spain) and (d) Rotliegend hydrocarbon reservoir in the Southern Permian Basin (The Netherlands). The facies models, combined with the analyses of the rock record, provides a comprehensive depositional framework where the influence of depositional characteristics, such as grain-size and sorting variations, interstitial clay distribution and composition and amount of intrabasinal components, on the extent and pathway of near-surface mechanical and chemical processes can be investigated. The particular dryland setting is characterized by prolonged periods of inactivity and short, episodic periods of peak discharge, which lead to the transport and deposition of poorly-sorted, clay-rich extra- and intraformational conglomeratic sediments upstream. Downstream, channels, mid-channel and bank-attached bars develop with conspicuous anisotropic trough and tabular cross-stratified sandstones. The most common near-surface diagenetic processes that alter the textural properties of these deposits are the rapid decrease of porosity and permeability due to grain-rearrangements and mechanical compaction of mud intraclasts along with pervasive early carbonate cementation. The results of this study will help to better configure the boundary conditions (e.g., external versus local supply for carbonates cements) in state-of-the-art reservoir quality forward models for ancient dryland river sandstones, which are especially prominent in Devonian, Permian, Triassic and Jurassic reservoir settings. © 2020
英文关键词	bank erosion; Devonian; diagenesis; paleoenvironment; permeability; Permian; porosity; reservoir characterization; sediment property; semiarid region; Triassic; Argana Basin; Guelmim-Oued Noun; Morocco
语种	英语
来源期刊	Earth Science Reviews
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/203734
作者单位	Department of Earth and Environmental Sciences, Division of Geology, KU Leuven, Celestijnenlaan 200E, Leuven, B-3001, Belgium; Department of Geoscience and Engineering, Delft University of Technology, Stevinweg 1, Delft, 2628CN, Netherlands; Friedrich - Alexander Universität, Lehrstuhl für Geologie, GeoZentrum Nordbayern, Schlossgarten 5, Erlangen, 91054, Germany
推荐引用方式 GB/T 7714	Henares S.,Donselaar M.E.,Caracciolo L.. Depositional controls on sediment properties in dryland rivers: Influence on near-surface diagenesis[J],2020,208.
APA	Henares S.,Donselaar M.E.,&Caracciolo L..(2020).Depositional controls on sediment properties in dryland rivers: Influence on near-surface diagenesis.Earth Science Reviews,208.
MLA	Henares S.,et al."Depositional controls on sediment properties in dryland rivers: Influence on near-surface diagenesis".Earth Science Reviews 208(2020).