干旱区生态环境知识资源中心(Arid): Sedimentology of a Permian playa lake: the Boda Claystone Formation, Hungary

Arid

DOI	10.2478/v10118-010-0002-1
	Sedimentology of a Permian playa lake: the Boda Claystone Formation, Hungary
	Konrad, Gyula; Sebe, Krisztina; Halasz, Amade; Babinszki, Edit
通讯作者	Sebe, K
来源期刊	GEOLOGOS
ISSN	1426-8981
EISSN	2080-6574
出版年	2010
卷号	16 期号:1 页码:27-41
英文摘要	The Upper Permian Boda Claystone Formation (BCF) in SW Hungary has been previously been identified as a saline lake deposit. A country-wide screening found this 800-1000 m thick succession the most suitable for the disposal of high-level radioactive waste in Hungary, and research into this formation has consequently been intensified since. The investigations included a detailed study of the sedimentological characteristics. Data obtained by mapping of the 25 km(2) outcrop area of the formation and from more than 40 boreholes were processed. The sedimentary structures were investigated on outcrop to microscopic scales, and cycles in the succession were interpreted. The main lithofacies, sedimentary structures and ichnofossils are presented. They indicate that the major part of the succession was deposited in a playa mudflat and is not of lacustrine origin in a strict sense. The lake sediments are represented by laminated and ripple-marked/flaser-type cross-laminated claystones and siltstones and by massive dolomites; trace fossils include crawling traces and burrows. Partial or complete drying out of the lake commonly occurred after the formation of carbonate mud by evaporation. Periodic fluvial influx is recorded by cross-bedded sandstones and unsorted gravelly sandstones of up to pebble-sized angular grains. Fenestral and stromatolitic structures reflect the repeated appearance of playa mudflat conditions. The silty claystones, which compose the major part of the succession, lost their primary structures due to pedogenic processes and indicate prolonged subaerial intervals with soil formation and only ephemeral inundations. The presence of pedogenic carbonate concretions supports the interpretation of an arid climate and a relatively shallow groundwater table. Drying-out events shown by desiccation cracks and authigenic breccias can be traced all over the succession. The various facies form small-scale sedimentary cycles showing a shallowing-upward trend and the growing influence of aridity and subaerial exposure.
英文关键词	Late Permian Boda Claystone Formation Hungary playa
类型	Article
语种	英语
开放获取类型	DOAJ Gold
收录类别	ESCI
WOS记录号	WOS:000434898500002
WOS类目	Geology
WOS研究方向	Geology
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/329593
作者单位	[Konrad, Gyula; Sebe, Krisztina] Univ Pecs, Dept Geol, Ifjusag U 6, H-7634 Pecs, Hungary; [Halasz, Amade] Univ Pecs, Inst Environm Sci, H-7634 Pecs, Hungary; [Babinszki, Edit] Geol Inst Hungary, H-1143 Budapest, Hungary
推荐引用方式 GB/T 7714	Konrad, Gyula,Sebe, Krisztina,Halasz, Amade,et al. Sedimentology of a Permian playa lake: the Boda Claystone Formation, Hungary[J],2010,16(1):27-41.
APA	Konrad, Gyula,Sebe, Krisztina,Halasz, Amade,&Babinszki, Edit.(2010).Sedimentology of a Permian playa lake: the Boda Claystone Formation, Hungary.GEOLOGOS,16(1),27-41.
MLA	Konrad, Gyula,et al."Sedimentology of a Permian playa lake: the Boda Claystone Formation, Hungary".GEOLOGOS 16.1(2010):27-41.