Salty brines on the Mediterranean sea floor

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Salty brines on the Mediterranean sea floor

机译：地中海海底的咸盐水

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In this communication, we report on brines from the Discovery Basin in the eastern Mediterranean which have the highest salinity ever found in the marine environment. They were formed by the dissolution of bischofite (MgCl_2.6H_2O) and filled the basin during the past 2,000 years. The brines give the first clear evidence for large-scale bischofite formation during the Messinian salinity crisis (late Miocene epoch, 5-6 million years ago) and demonstrate that the eastern Mediterranean became evaporated to near dryness during this time.

机译：在此通讯中，我们报告了地中海东部发现盆地的盐分，这些盐分是海洋环境中盐度最高的。它们是由Bischofite（MgCl_2.6H_2O）溶解形成的，并在过去2,000年中充满了盆地。这些盐水为在墨西尼盐度危机（中新世晚期，5-6百万年前）期间大规模的重辉铁矿形成提供了第一个明确的证据，并表明在此期间东地中海已蒸发至接近干燥。

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《Nature》 |1997年第6628期|p.31-32|共2页
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收录信息美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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正文语种 eng
中图分类自然科学总论;
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4. Hydrochemistry Research of Intercrystalline with Pore Brine and Pre-3D Modelling of Heibeiwadi Brine Deposit [C] . Huang Song International Conference on Material Science and Engineering . 2018

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5. Calcium isotopic variation in marine evaporites and carbonates: Applications to late Miocene Mediterranean brine chemistry and late Cenozoic calcium cycling in the oceans. [D] . Hensley, Tabitha Michele. 2006

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机译：关于富含甲烷的热盐水的Aheratigenic碳酸盐在Cheops Mud火山中，Menes Caldera（尼罗河深海粉丝，东地中海）

Salty brines on the Mediterranean sea floor

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