Phases of Magmatic Activities in South Wadi Hodein-Shalatein, Egypt: Resolving controversy about their age using Paleomagnetism and AMS

A. Awad, Esmat Abd El-Aal, Ahmed Amin Khashaba
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Abstract

ABSTRACT Several exposures of basaltic intrusions are distributed near Red Sea coast at Wadi Hodein Southern Egypt. There is some disagreement about the palaeomagnetic pole results of these basalts; some claim it is Tertiary in age, while others claim it is of Cretaceous age. To our knowledge, no Anisotropy of Magnetic Susceptibility (AMS) results have ever been published from these rocks. Therefore, palaeomagnetic and AMS studies were performed on these basalts in order to identify phases of magmatism, paleomagnetic pole position and types of magmatic intrusions. In the present study, eight sites (219 oriented core specimens) were sampled from eight location. Rock magnetic studies reflect the presence of magnetite as the chief mineral in these rocks. Alternating field technique in association with Thermal Demagnetisation process revealed presence of one magmatic phase took place in Cretaceous age with VGP (65°N, 250°E; A 95 = 5.3). AMS results showed that the basaltic intrusions in the study area are still holding their primary fabrics.
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埃及南Wadi Hodein-Shalatein岩浆活动的阶段:利用古地磁和AMS解决岩浆活动年龄的争议
摘要:在埃及南部瓦迪霍德恩的红海海岸附近分布着几处玄武岩侵入体。这些玄武岩的古磁极结果存在一些分歧;有人说它是第三纪的,也有人说它是白垩纪的。据我们所知,这些岩石的磁化率各向异性(AMS)结果尚未发表。因此,对这些玄武岩进行了古地磁和AMS研究,以确定岩浆活动的阶段、古磁极位置和岩浆侵入类型。本研究在8个地点采集了8个样点(219个定向岩心标本)。岩石磁学研究反映了这些岩石中的主要矿物是磁铁矿。结合热退磁过程的交变场技术揭示了白垩纪时期VGP(65°N, 250°E)存在一个岩浆相;A 95 = 5.3)。AMS结果表明,研究区玄武岩侵入体仍保持其原始构造。
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