CRETACEOUS - PALEOGENE SEQUENCE STRATIGRAPHY OF THE LEVANT PLATFORM (EGYPT, SINAI, JORDAN)

机译：左旋平台的白垩纪-古近纪层序地层（埃及，西奈，约旦）

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This contribution represents a summary of our interdisciplinary studies of the Cretaceous-Paleogene Levant Platform (LP) to reconstruct the factors controlling its growth and geometry. We define six platform units (PU1, PU2a, b, PU3 and PU4a, b) based on facies characteristics. Four key surfaces are defined that occur elsewhere in the LP and are of North African or Tethyan importance. They are due to prominent changes of the tectonic or paleoceanographic regimes. Stacking patterns of Aptian to Paleogene platform units and important surfaces are defined within a biostratigraphic frame and allow to interprete a total number of 35 third-order depositional sequences, some of which have been amalgamated locally. Comparisons of our sea level charts with those from neighbouring platforms indicate several mismatches that may be due to local uplift, subsidence, or increasing clastic input.

机译：这一贡献代表了我们对白垩纪-古近纪黎凡特平台（LP）的跨学科研究的总结，以重建控制其生长和几何形状的因素。我们根据相特征定义了六个平台单元（PU1，PU2a，b，PU3和PU4a，b）。 LP中定义了四个关键表面，这些表面具有北非或Tethyan的重要性。它们是由于构造或古海洋学制度的显着变化。在生物地层学框架内定义了Aptian到古近纪平台单元和重要表面的堆积模式，并可以解释总共35个三阶沉积序列，其中一些已经局部合并。将我们的海平面图与邻近平台的海平面图进行比较，可以发现一些不匹配的情况，这可能是由于局部隆起，沉降或碎屑输入增加所致。

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《NATO Advanced Research Workshop on North African Cretaceous Rudist and Coral Formations and their Contributions to Carbonate Platform Development; May 13-18, 2002; Tunis, Tunisia》|2002年|p.171-187|共17页
会议地点 Tunis(TN)
作者
J. KUSS; A. BASSIOUNI; J. BAUER; M. BACHMANN; A. MARZOUK; C. SCHEIBNER; F. SCHULZE;
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FB5 Geowissemchaften, Universitaet Bremen, P.O. Box 330440, D-28334 Bremen, Germany;

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原文格式 PDF
正文语种 eng
中图分类地质学;
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CRETACEOUS - PALEOGENE SEQUENCE STRATIGRAPHY OF THE LEVANT PLATFORM (EGYPT, SINAI, JORDAN)

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