亚德里亚东部被动边缘的演化记录在阿尔卑斯山脉和迪纳里德斯山脉过渡带的浅-深水序列中(Ivanščica Mt.， NW Croatia)

IF 1.8 3区地球科学 Q1 GEOLOGY

Facies Pub Date : 2023-10-01 DOI:10.1007/s10347-023-00674-7

Matija Vukovski, Duje Kukoč, Tonći Grgasović, Ladislav Fuček, Damir Slovenec

引用次数: 0

摘要

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Evolution of eastern passive margin of Adria recorded in shallow- to deep-water successions of the transition zone between the Alps and the Dinarides (Ivanščica Mt., NW Croatia)

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Evolution of eastern passive margin of Adria recorded in shallow- to deep-water successions of the transition zone between the Alps and the Dinarides (Ivanščica Mt., NW Croatia)

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来源期刊

Facies 地学-地质学

CiteScore

3.70

自引率

5.60%

发文量

审稿时长

>12 weeks

期刊介绍： The journal is open to papers dealing with the interpretation of ancient and modern biotopes and carbonate depositional environments by means of facies analysis in its broadest sense. Once the central part of research in hydrocarbon exploration, facies analysis more and more integrates modern and ancient biogeological processes of a changing earth. Special emphasis is laid on paleobiology and -ecology, basin evolution, sedimentology including diagenesis and geochemistry, as well as studies emphasising the impact of life on earth history. The main part of the target group will be people in academia.