奥克尼Westray中泥盆纪-上Stromness Flagstone和Rousay Flagstone地层之间边界的划分

IF 0.5 4区 地球科学 Q4 GEOLOGY
D. Leather
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引用次数: 2

摘要

只有地质调查局在1932年和1935年发布的官方地图显示了奥克尼上中泥盆纪Stromness和Rousay Flagstone之间的边界。从那时起,定义和定位这一边界的困难就对奥尔卡迪安湖流域的许多工人提出了挑战。2015年,Uisdan Michie根据鱼类化石引入了生物带,最近在Westray岛上一个突出的海床中发现了该生物带化石Osteolepis pandri和Thursius pholidotus,这使得Rousay组底部的边界可以在奥克尼的这一地区确定。有人建议,这种有节奏的沉积物循环的海床的其他特征,以及相邻循环中的特征,可以作为进一步对比和绘制整个流域地图的标志。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Demarcation of the boundary between Middle Devonian Upper Stromness Flagstone and Rousay Flagstone formations in Westray, Orkney
The only official maps to show a boundary between the Middle Devonian Stromness and Rousay Flagstones on Orkney are those published by the Geological Survey in 1932 and 1935. Since then, the difficulties of defining and locating this boundary have challenged many workers in the Orcadian Lake Basin. In 2015, the introduction of biozones by Uisdean Michie, based on fossil fish, and the recent discovery in Westray of the zone fossils Osteolepis panderi and Thursius pholidotus in a prominent fish bed across the island, has permitted the boundary for the base of the Rousay Formation to be determined in that part of Orkney. It is suggested that other characteristics of the fish bed of this rhythmic cycle of sediments, together with those in adjacent cycles, may be used as a marker for further correlation and mapping across the basin.
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来源期刊
Scottish Journal of Geology
Scottish Journal of Geology 地学-地质学
CiteScore
1.70
自引率
0.00%
发文量
10
审稿时长
>12 weeks
期刊介绍: Although published only since 1965, the Scottish Journal of Geology has a long pedigree. It is the joint publication of the Geological Society of Glasgow and the Edinburgh Geological Society, which prior to 1965 published separate Transactions: from 1860 in the case of Glasgow and 1863 for Edinburgh. Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology. The diverse geology of Scotland continues to provide an important natural laboratory for the study of earth sciences; many seminal studies in geology have been carried out on Scottish rocks, and over the years the results of much of this work had been published in the Journal and its predecessors. The Journal fully deserves its high reputation worldwide and intends to maintain its status in the front rank of publications in the Earth sciences.
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