气候变化领域集成服务门户(CCPortal): Chlorite in sandstones

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DOI	10.1016/j.earscirev.2020.103105
	Chlorite in sandstones
	Worden R.H.; Griffiths J.; Wooldridge L.J.; Utley J.E.P.; Lawan A.Y.; Muhammed D.D.; Simon N.; Armitage P.J.
发表日期	2020
ISSN	00128252
卷号	204
英文摘要	Chlorite, an Fe- and Mg-rich aluminosilicate clay, may be either detrital or authigenic in sandstones. Detrital chlorite includes mineral grains, components of lithic grain, matrix and detrital grain coats. Authigenic chlorite may be grain-coating, pore-filling or grain-replacing. Chlorite can be observed and quantified by a range of laboratory techniques including light optical and scanning electron microscopy and X-ray diffraction; the presence of chlorite in sandstone can be identified by the careful integration of signals from downhole logs. Grain-coating chlorite is the only type of chlorite that can help sandstone reservoir quality since it inhibits quartz cementation in deeply buried sandstones. Grain coats are up to about 10 μm thick and typically isopachous on all grain surfaces; they result from rapid indiscriminate nucleation at high levels of chlorite supersaturation in the pore waters and then growth of appropriately oriented nuclei as ultra-thin, roughly equant crystals. Chlorite can have many possible origins, but it is likely that grain-coating chlorite results from closed system diagenesis at the bed scale. Chlorite sources include transformation of detrital Fe-rich berthierine, transformation of Mg-rich smectite, reaction of kaolinite with sources of Fe and breakdown of volcanic grains. The specific origin of chlorite controls its composition, with chlorite in marine sandstones having a berthierine source and chlorite in continental sandstones having a smectite source. Incorporation of precursor clays required for chlorite growth can be achieved by a variety of processes; these most commonly occur in marginal marine environments possibly explaining why Fe-rich chlorite coats are most commonly found in marginal marine sandstones. © 2020 The Authors
关键词	Burial diagenesis Cement Chlorite Delta Eodiagenesis Estuary Grain-coating Mesodiagenesis Pore-filling Pyrite Quartz-inhibition Reservoir quality Sandstone Sedimentary environment, petrophysics Siderite Wireline log
英文关键词	aluminosilicate; authigenic mineral; cementation; chlorite; clay mineral; detrital deposit; diagenesis; iron; magnesium; marine sediment; sandstone
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/203932
作者单位	Department of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool, L69 3GP, United Kingdom; BP Exploration, Chertsey Road, Sunbury-on-Thames, Middlesex, TW16 7LN, United Kingdom; BP Upstream Technology, Chertsey Road, Sunbury-on-Thames, Middlesex, TW16 7LN, United Kingdom; Department of Geology, Bayero University, Kano State, Nigeria
推荐引用方式 GB/T 7714	Worden R.H.,Griffiths J.,Wooldridge L.J.,et al. Chlorite in sandstones[J],2020,204.
APA	Worden R.H..,Griffiths J..,Wooldridge L.J..,Utley J.E.P..,Lawan A.Y..,...&Armitage P.J..(2020).Chlorite in sandstones.Earth Science Reviews,204.
MLA	Worden R.H.,et al."Chlorite in sandstones".Earth Science Reviews 204(2020).