A marker band folgen stratigraphy for the Cenomanian Chalk of England and its extension to northen Germany and France

IF 1.1 4区 地球科学 Q3 GEOLOGY
Christopher Vincent Jeans
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引用次数: 0

Abstract

: Jeans, C.V. 2023. A marker band folgen stratigraphy for the Cenomanian Chalk of England and its extension to northen Germany and France. Acta Geologica Polonica , 73 (2), 135–180. Warszawa. A novel stratigraphical scheme within the Folge Concept is described for the Cenomanian Chalk of England that is particularly suitable for investigating the regional changes in the lithofacies, diagenesis, geochemistry, and mineralogy of the sediments of the Chalk Sea leading up to the Cenomanian–Turonian Oceanic Anoxic Event. It is based on “isochronous” marker bands defined largely by calcitic macrofossil assemblages, and it avoids problems caused by the poor or non-preservation of ammonite assemblages and lateral changes in chalk lithofacies. Eight folgen are based on one, two, or more marker bands. Their sequences, lithologies and calcitic macrofossil assemblages are described from 33 exposures in the Northern Chalk Province of England. The folgen are named, in ascending order, the Belchford, Stenigot, Dalby, Bigby, Candlesby, Nettleton, Louth and Flixton, after villages in Lincolnshire and Yorkshire, England. The folgen are traced throughout the Transitional and Southern Chalk provinces of England. They are present in the Cenomanian chalk of northern Germany and northwest France. Regionally, an individual folge may display considerable vertical and lateral variation in general lithology and lithofacies whilst still maintaining their defining marker bands. The possibility of further refinement to the scheme is discussed.
英格兰Cenomanian白垩系的标志带folgen地层学及其延伸至德国和法国北部
:牛仔裤,简历2023。英国塞诺曼尼亚白垩系的标志带褶皱地层及其向德国和法国北部的延伸。地质学报,73(2),135-180。华沙。在Folge概念中描述了一种新的地层方案,该方案特别适用于研究白垩海沉积物的岩相、成岩作用、地球化学和矿物学的区域变化,从而导致了Cenomanian - turonian海洋缺氧事件。它基于主要由钙质大化石组合确定的“等时”标志带,避免了由于鹦鹉螺组合保存不良或未保存以及白垩岩相横向变化造成的问题。八个folgen是基于一个,两个或更多的标记带。本文描述了英国北部白垩省33处暴露物的层序、岩性和钙质大化石组合。福尔根按升序依次被命名为Belchford, Stenigot, Dalby, Bigby, Candlesby, Nettleton, Louth和Flixton,分别来自英格兰林肯郡和约克郡的村庄。folgen在英格兰的过渡时期和南部白垩省都有迹可寻。它们存在于德国北部和法国西北部的塞诺曼尼亚白垩中。从区域上看,一个单独的岩性和岩相可能在纵向和横向上表现出相当大的变化,但仍保持其明确的标志带。讨论了进一步改进该方案的可能性。
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来源期刊
Acta Geologica Polonica
Acta Geologica Polonica 地学-地质学
CiteScore
1.70
自引率
18.20%
发文量
0
审稿时长
>12 weeks
期刊介绍: Acta Geologica Polonica publishes original and review papers on all aspects of basic geology, with particular focus on sedimentology, stratigraphy, palaeontology, regional geology, structural geology, and regional petrography. All papers are published in English.
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