The Carbonate Platforms of Neotethys: a Comparison Study between Apulia and Eratosthenes Platforms

V. Kosmidou, N. Papadimitriou
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Abstract

Summary Apulian Platform has been developed on the passive margin of Africa, the Adria or Apulia margin. It is characterised by platforms and deep-sea basins controlled by the Norian-Liassic rifting phase of the Tethyan rifting (Bertottti, 1993). The Eratosthenes carbonate platform sits on top of a thicker continental block (Moho depths of 32–35 km, Feld et al. 2017) compared to adjacent basins and would thus have been subject to lower rates of subsidence than the Levant Basin ( Gardosh et al., 2010 ). This differential subsidence between crustal segments of different nature is well described for other Mediterranean passive margins. The Eratosthenes and Apulian platforms remain wholly carbonate (“clean”). Seismic interpretation suggests that the infilling adjacent to both the Eratosthenes and the Apulia carbonate platform consists of gravity and mass transport complexes (MTCs) as well as deep pelagic sediments that onlap the paleo-slopes of the Mesozoic platforms. The mechanisms that triggered these large slope failures (maximum width 15–30 km) could be a combination of several parameters including (a) rapid sedimentary loading that can generate excess pore pressure, (b) earthquakes associated with the major geodynamic events, and (c) erosion of older successions due to fluctuations in sea level.
新特提斯碳酸盐岩台地:阿普利亚台地与埃拉托色尼台地的比较研究
阿普利亚地台是在非洲被动边缘、亚德里亚或阿普利亚边缘发育的。它的特点是台地和深海盆地受特提斯裂谷的Norian-Liassic裂谷期控制(Bertottti, 1993)。与邻近盆地相比,Eratosthenes碳酸盐岩台地位于较厚的大陆块体(Moho深度为32-35 km, Feld et al. 2017)的顶部,因此沉降率低于Levant盆地(Gardosh et al., 2010)。不同性质的地壳段之间的这种差异沉降在地中海其他被动边缘也有很好的描述。埃拉托色尼台地和阿普利亚台地仍然完全是碳酸盐(“干净的”)。地震解释表明,埃拉托色尼台地和阿普利亚碳酸盐岩台地附近的充填物由重力和物质搬运复合体(mtc)以及覆盖在中生代台地古斜坡上的深海沉积物组成。触发这些大型边坡破坏(最大宽度15-30公里)的机制可能是几个参数的组合,包括(a)可能产生超孔隙压力的快速沉积载荷,(b)与主要地球动力学事件相关的地震,以及(c)由于海平面波动而导致的较旧序列的侵蚀。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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