Pedogenic calcrete records in southern Transdanubia, Hungary : a brief review with paleoenvironmental and paleogeographic implications

A. Varga, B. Raucsik
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引用次数: 4

Abstract

In the Hungarian part of the Tisia Block, four occurrences of rhizolith-bearing pedogenic calcrete have been published, three of which are located in southern Transdanubia. Nodular calcrete with beta fabrics was documented from the lower Permian (Cisuralian) continental Korpad Sandstone Formation where the subaerial exposure section was developed on a strongly altered, volcanic shard-rich siliciclastic substrate. Additionally, two locations with Microcodium-bearing calcrete developed on a lower Jurassic carbonate substrate were published in the last few years. The scope of this study is to briefly summarize pedogenic calcrete records known from the Permian to the Cenozoic of southern Transdanubia (Tisia Block, Hungary), and to highlight their regional paleoenvironmental and paleogeographic importance.
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匈牙利外多瑙河南部成土钙质记录及其古环境和古地理意义
在Tisia地块的匈牙利部分,已发表了四处含根茎石的成土钙质,其中三处位于外多瑙河南部。在下二叠世(顺拉纪)陆相Korpad砂岩组中发现了带有β结构的结节状钙质,该组的陆上暴露剖面发育在一个强烈蚀变的、富含火山碎屑的硅屑基底上。此外,在过去的几年里,在下侏罗统碳酸盐岩基底上发现了两个含微钴钙砾岩的位置。本研究的范围是简要总结外多瑙河南部(匈牙利Tisia地块)二叠纪至新生代的成土钙质记录,并强调其在区域古环境和古地理上的重要性。
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来源期刊
Central European Geology
Central European Geology Earth and Planetary Sciences-Geology
CiteScore
1.40
自引率
0.00%
发文量
8
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