Geochemical studies on the Feshcha Springs, Dead Sea basin
Geochemical studies on the Feshcha Springs, Dead Sea basin
复制标题
死海盆地 Feshcha Springs 的地球化学研究
DOI：
10.1016/0022-1694(72)90074-1
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发表时间：
1972
影响因子：
6.4
通讯作者：
M. Molcho
中科院分区：
文献类型：
--
作者：
E. Mazor;M. Molcho
菲什哈温泉位于死海岸边4公里长的狭长地带。它们构成两个独立的组：a) T-N水，其盐成分、温度和氡含量与裂谷“提比里亚-诺伊特水协会”的许多其他成员相似。水文学、氡、氚和碳-14表明，它们是最近的大气水与至少有18000年历史的古代（被困的）T-N水的混合物。b) Z-Y水域，像死海盆地的其他成员“Zohar-Yesha水群”一样，起源于T-N水域与死海水域的混合。这可以从化学成分中看出，并由氧-18和氘的数据证实。
The Feshcha springs issue in a 4 km long strip on the Dead Sea shores. They constitute two separate groups: a) T-N waters, similar in their salt composition, temperature and radon content to the many other members of the Rift Valley “Tiberias-Noit water association”. The hydrologic, radon, tritium and carbon-14 indicate they are mixtures of recent meteoric waters with ancient (trapped) T-N waters of an age of at least 18000 years. b) Z-Y waters which, like other members of the Dead Sea basin “Zohar-Yesha water group”, originate by a mixing of T-N waters with Dead Sea waters. This is seen in the chemical compositions and is confirmed by the oxygen-18 and deuterium data.