莫利塞-阿普利亚底土中的上新世和上新世碎屑灰岩层

IF 1.6 3区地球科学 Q2 GEOLOGY

Rivista Italiana Di Paleontologia E Stratigrafia Pub Date : 2020-05-08 DOI:10.54103/2039-4942/13431

R. Casnedi, A. Balduzzi

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引用次数: 0

摘要

莫利塞和阿普利亚地下勘探在中生代-中新世碳酸盐序列顶部和中新世浊积岩内发现了碎屑钙质层。前者是喀斯特裂隙和构造高地挤压的结果，后者是断层斜坡底部大量流动的结果。在浊积岩中，一个生物钙钛矿地层是一个很好的电标记，证明了陆架的形成。它与亚平宁山脉广泛发育的中新世缺口相对应。

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LIVELLI CALCAREI CLASTICI DEL MIOCENE SUPERIORE E PLIOCENE NEL SOTTOSUOLO MOLISANO-PUGLIESE

The Molise and Apulia subsurface exploration has found clastic calcareous layers at the top of the Mesozoic—Miocene carbonate sequence and within the Middle Pliocene turbidites. The first are the result of Karst—fissures and crushing on the structural highs and mass flows at the base of fault slopes. Within the turbidites a biocalcarenitic horizon IS an electric good marker which proves an event of a shelf build up. It corresponds to the Middle Pliocene gap widely developed in the Apennines.

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来源期刊

Rivista Italiana Di Paleontologia E Stratigrafia 地学-地质学

CiteScore

3.60

自引率

4.30%

发文量

审稿时长

>12 weeks

期刊介绍： The Rivista Italiana di Paleontologia e Stratigrafia was founded in 1895. It publishes original papers dealing with all fields of paleontology and of stratigraphy, from Italy and the Mediterranean to the Tethys, as well across the globe from China to North America.