首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >The western edge of the Mediterranean Pelagian Platform: A Messinian mixed siliciclastic-carbonate ramp in northern Tunisia
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The western edge of the Mediterranean Pelagian Platform: A Messinian mixed siliciclastic-carbonate ramp in northern Tunisia

机译:地中海Pelagian平台的西边缘:突尼斯北部的一个墨西尼混合硅质碎屑碳酸盐岩斜坡

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摘要

The marine Messinian deposits of Tunisia cover a narrow littoral strip some 300 km long between the northern Bizerte and Cap Bon areas and the central-eastern Sahel region. Litho- and biofacies analysis of six stratigraphic sections reveals the distinctive features of these deposits. The lower Messinian deposits are characterized by ubiquitous siliciclastics and abundant oolitic/bioclastic limestones organized in an eastward facing ramp. Westward (landward), this ramp changes into coastal lagoons, sometimes containing evaporites. Eastward, the ramp passes to the reefal Pelagian Platform extending as far as Lampedusa. Two main sedimentary cycles are distinguished: 1) an early Messinian siliciclastic retrogradational then oolitic/bioclastic progradational cycle (Beni Khiar Formation and lower Oued bel Khedim Formation): 2) a late Messinian brackish to continental cycle that probably accumulated in rapidly subsiding lagoons (Cued el Bir Formation and upper Oued bel Khedim Formation). The Tunisian early Messinian cycle is partly eustatically controlled, but the late Messinian cycle cannot be confidently correlated to other well-known Messinian series because of tectonic movements. The lower Messinian deposits of Tunisia are also characterized by abundant suspension-feeding organisms (molluscs and bryozoans) and rare corals, calcareous algae, echinoids, and larger benthic foraminifers. The proposed palaeoenvironmental model shows that the lower Messinian ramp of Tunisia was located on a current-protected margin and subjected to continent-derived sediment and nutrient supply. Eastward, nutrient influx diminished and a shallow-water isolated carbonate platform with coralgal facies developed between the western and the eastern Mediterranean basins. The main hydrological connection between these two basins occurred through a narrow seaway situated to the northeast of the Pelagian Platform, south of Sicily and Malta.
机译:突尼斯的海洋墨西尼沉积物覆盖了一条狭窄的沿海地带,介于比塞大北部和Cap Bon地区与萨赫勒地区中东部之间约300公里。对六个地层的岩相和生物相分析揭示了这些矿床的独特特征。墨西拿下部矿床的特征是在朝东的斜坡上分布着无处不在的硅质碎屑岩和大量的橄榄岩/生物碎屑灰岩。向西(向西),该坡道变为沿海泻湖,有时包含蒸发岩。向东,坡道到达珊瑚礁的Pelagian平台,一直延伸到Lampedusa。有两个主要的沉积周期:1)早期的墨西尼硅质碎屑逆行然后是卵质/生物碎屑的演化周期(贝尼·基亚尔组和下乌德贝勒·赫迪姆组):2)墨西尼后期的微咸至大陆性周期,可能在快速沉降的泻湖中积累(提示)。 El Bir组和上Oued bel Khedim组)。突尼斯的早期墨西尼周期部分受地心控制,但由于构造运动,后期的墨西尼周期不能与其他著名的墨西尼阶相关。突尼斯的较低的麦西尼亚沉积物还具有大量的以悬浮物为食的生物(软体动物和苔藓动物)和稀有的珊瑚,钙质藻类,棘突类动物和较大的底栖有孔虫。所提出的古环境模型表明,突尼斯的墨西尼下部斜坡位于受电流保护的边缘,并受到大陆衍生的沉积物和营养物的供应。向东,养分流入减少,并且在地中海盆地的东部和西部之间形成了浅水孤立的碳酸盐台地,并形成了珊瑚相。这两个盆地之间的主要水文联系是通过位于西西里岛和马耳他南部Pelagian平台东北部的一条狭窄航道发生的。

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