Alnawafleh, H., Tarawneh, K., Ibrahim, K., Zghoul, K., Titi, A., Rawashdeh, R., Moumani, K. and Masri, A. (2015) Characterization and Origin of the Miocene Mudawwara-Quwayra Basaltic Dike, Southern Jordan. International Journal of Geosciences, 6, 869-881.
https://doi.org/10.4236/ijg.2015.68071

has been cited by the following article:

• TITLE: Petrography, Geochemistry and Petrogensis of Pleistocene Basaltic Flow from Northwest Atarous Area, Central Jordan

  AUTHORS: Hassan Al-Fugha, Ibrahim Ahmad Ali Bany Yaseen

  KEYWORDS: Petrography, Geochemistry, Petrogensis, Pleistocene Basaltic, Atarous Basalt, Jordan

  JOURNAL NAME: International Journal of Geosciences, Vol.10 No.6, June 11, 2019

  ABSTRACT: Fifteen basaltic rock samples were collected from central Jordan at the Atarous volcanism basaltic flow area. The samples cover about 8 km2 from the Atarous Basalt flow (AB). The AB flow was introduced in the Miocene to Pleistocene periods. The samples analyze major and trace elements by using XRF. Petrography, Geochemistry and Petrogensis have investigation to carried out for the AB. The petrography analyses of the AB rocks show they are composed of plagioclase (labradorite and bytownite), pyroxene (augite), and olivine (forsterite); accessory minerals include apatite and secondary minerals magnetite, ilmenite, spinel and iddingsite. The AB is classified within alkaline to sub-alkaline and tholeiitic to Calc-Alkaline basalt. The Mg# range between 0.39 and 0.49 of basalt samples exhibits different degrees of fractionation with a low degree of melting