Petrography, Geochemistry and Petrogenesis of the Basalt Flow at Al Azraq Al Shamali Area, East Jordan

Ibrahim Ahmad Bany Yaseen, Abd Alkareem Eefan Al Smairan
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Abstract

Al Azraq Al Shamali (AZS) basaltic rocks were investigated aiming to under-stand their mineralogy, petrography and geochemistry features, and to achieve that a total of sixteen representative rock samples were selected for both geochemical and petrographic analysis from several sites in the study area. Petrographic characteristics were analyzed by optical microscopy after preparation thin sections for representative rock samples, which show that all basalt samples have minerals comprising: olivine, plagioclase (labradorite), clinopyroxene (augite), opaque’s and some secondary minerals such as Iddingsite, however, the proportions of each mineral vary between samples. Normative mineralogy by using CIPW Norm showed that AZS basalt samples dominated by olivine, Diopside, and nepheline, and AZS basalt can be normatively classified as alkali olivine basalt. Some textures that may be evident on microscopic examination such as porphyritic, glomeroporphyritic, vesicular, intergranular, and ophitic to sub-ophitic texture. X- Ray Fluorescence was used for whole rock major elements analysis (SiO 2 , TiO 2 , Al 2 O 3 , Fe 2 O 3 , MnO, MgO, CaO, Na 2 O, K 2 O
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东约旦Al Azraq Al Shamali地区玄武岩流的岩石学、地球化学及岩石成因
对Al Azraq Al Shamali (AZS)玄武岩进行了研究,目的是了解其矿物学、岩石学和地球化学特征,并从研究地区的几个地点共选择了16个具有代表性的岩石样品进行地球化学和岩石学分析。对代表性岩石样品进行薄片制备后的岩石学特征进行了光学显微镜分析,结果表明,所有玄武岩样品均含有橄榄石、斜长石(labradorite)、斜辉石(augite)、不透明矿物和一些次生矿物如Iddingsite,但每种矿物的比例在样品之间有所不同。CIPW Norm规范矿物学分析表明,AZS玄武岩样品以橄榄石、透辉石和霞石为主,可归为碱性橄榄岩玄武岩。镜下可见一些结构,如卟啉质、肾小球卟啉质、水泡状、粒间质和蛇至亚蛇啉质。采用X射线荧光法对全岩主要元素(sio2、tio2、al2o3、fe2o3、MnO、MgO、CaO、Na 2o、k2o)进行了分析
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