litosphereЛитосфераLITHOSPHERE (Russia)1681-90042500-302XA.N. Zavaritsky Institute of Geology and Geochemistrylitosphere-573Research ArticleСтатьиArticlesМагматизм Махтеш Рамона: геология, геохимия, петрогенезис (природоохранная зона хар Ха-Негев, Израиль)ЮдалевичЗ. А.noemail@neicon.ruФерштатерГерман Борисовичfershtater@igg.uran.ruЭйяльМ. .noemail@neicon.ruУниверситет Бен ГурионаRussian FederationИнститут геологии и геохимии УрО РАНRussian Federation201415022019037092Copyright © Юдалевич З.А., Ферштатер Г.Б., Эйяль М..., 20192019Юдалевич З.А., Ферштатер Г.Б., Эйяль М...Юдалевич З.А., Ферштатер Г.Б., Эйяль М...Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.lithosphere.ru/jour/article/view/573

Раннемеловые магматические породы котловины Махтеш Рамон (пустыня Негев, Израиль), среди которых преобладают щелочные оливиновые базиты, образуют две группы, разделенные конгломератами Arod, залегающими в основании формации Hatira I (нижняя). Ранняя группа - предконгломератовая (РreArod сgl) - представлена базальтами Сахароним и бимодальной габбро(базальт)-сиенитовой серией, а поздняя - (PostArod сgl) - базальт-базанит-нефелинитовой серией. Породы образуют лавовые потоки, дайки, силлы, некки. Они отвечают геодинамическому типу внутриплитных рифтогенных континентальных базальтов. По петрологическим и геохимическим особенностям породы РreArod сgl группы близки к постщитовой серии Гавайских островов, а породы базальт-базанит-нефелинитовой к постэрозионной серии этих островов. PostArod сgl ассоциация, кроме того, очень близка к континентальной базальт-базанит-нефелинитовой части серии Балконес в США. В качестве магматического источника пород предполагается участие метасоматизированной мантии, представленной ксенолитами железистых верлитов в базанитах.

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The authors declare that there are no conflicts of interest present.