Volume 5, Issue 6, December 2016, Page: 82-95
Mineralogy, petrology and Geochemistry of the Basalt flows at Ash-Shun Ash-Shamaliyya Area, North West Jordan
Ibrahim Ahmad Ali Bany Yaseen, Institute of Earth and Environmental Sciences, Al al-BaytUniversity, Mafraq, Jordan
Alaa Yaser Abidrabbu, Institute of Earth and Environmental Sciences, Al al-BaytUniversity, Mafraq, Jordan
Received: Aug. 29, 2016;       Accepted: Oct. 5, 2016;       Published: Nov. 7, 2016
DOI: 10.11648/      View  5650      Downloads  282
Twenty-seven basaltic fresh rock samples collected from North West Jordan at Ash-Shuna Ash-Shamaliyya area studied. The Ash-Shuna Ash-Shamaliyya basalt (SHB) introduced within Pliocene to Quaternary (recent) volcanism in North West Jordan, and produced within intraplate continental alkali to calc-alkaline basalt. The mineralogy analyses of the SHB rocks are composed of plagioclase, pyroxene, olivine, opaque minerals (iron oxide), and secondary minerals included iddingsite and calcite. The common textures of the SHB were trachytic, glomeroporphyritic, seriate, intergranular, poikilitic, corona, ophtic to subophitic, radiate, cumulate, vesicular and amygdaloidal. The geochemical analysis data of SHB indicated that SHB was derived from a slightly fractionation magma as reflected by high MgO concentration(average 8ppm) and Mg#% (average 46%), and high concentration Ni (average158ppm) and low silica content (average 48wt%). The Geochemical classification of SHB introduced within basaltic to trachybasalt field and calc-alkaline to alkali basalt. The tectonic setting of SHB explained by using discrimination diagrams, Ti-Zr-Y, Ti-Zr-Sr, MgO-FeO(tot)-Al2O3, and Nb-Y, the SHB plotted within plate, calc-alkali and continental basalt respectively. The Rayleigh fractionation equation modeled for Sr verses Ba vector diagram indicated the SHB had fractionation less than10% for clinopyroxene, orthpyroxene, olivine and plagioclase.
Calc-Alkaline Basalt, Tectonic Setting, Fractionation, Ash-Shuna Ash-Shamaliyya, Jordan
To cite this article
Ibrahim Ahmad Ali Bany Yaseen, Alaa Yaser Abidrabbu, Mineralogy, petrology and Geochemistry of the Basalt flows at Ash-Shun Ash-Shamaliyya Area, North West Jordan, Earth Sciences. Vol. 5, No. 6, 2016, pp. 82-95. doi: 10.11648/
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Abderahman, N. and El- Akhal, H., 2004: Mineralogical composition of Jordan and its physical properties as construction material. ABHATHAL-YARMOUK:"Basic Sci. &Eng., V.13,pp. 283-300.
Al- Malabeh, A., 2015: Geological Location map of Basalt flows in north Jordan. Yarmouk University, Department of the Earth and environmental sciences, Irbid Jordan.
Al-Malabeh, A.,2003:Geochemistry and Volcanology of Jabal Al-Rufiy at, Strombolian Monogenic Volcano, Jordan. Dirasat, V.30, pp. 125-140.
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, V.6, pp.869-881.
Bany Yaseen I. A. A., 2016: Petrography, Geochemistry and Petrogensis of Basal Flow from Ar-Rabba Area, Central Jordan, International Journal of Geosciences, V.7, pp.378-396,
Bany Yaseen, I. A. A. 2014: Contribution to the Petrography, Geochemistry, and Petrogenesis of Zarqa-Ma’in Pleistocene Alkali Olivine Basalt Flow of Central Jordan, International Journal of Geosciences, V.5, pp.657-672.
Barberi, F., Capaldi ,G., Gasperini, P., Marinelli,G., Santacroce, R., Scandone, R., Treuil, M. and Varet, J., 1979: Recent Basaltic Volcanism of Jordan and Its Implications on the Geodynamic Evolution of the Afro-Arabian Rift System. Academia Nazionale DeiLincei, Att DelConvegni Lincei, Rome, pp. 667-683.
Basem K., 2000: Geological Map of Ash-Shuna Ash-Shamaliyya, Natural Resources Authority (NRA), Geology Directorate, Amman, Jordan.
Bender, F., 1974: Geology of the Arabian Peninsula, Jordan. US Geological Survey Professional Paper, V.36, pp.560-561
Camp, V. and Roobol, M., 1992: Upwelling Asthenosphere Beneath Western Arabian and Its Regional Implication. Journal of Geophysical Research, V.97, pp.15255-15271.
Camp V. E. and M. J. Roobol. (1989):Upwelling Asthenosphere Beneath Western Arabia and Its Regional Implications, Journal of Geophysical Research, 255-271.
Colemann, R. G., Gregory, R. T., and Brown,G. R.,1983:Cainozoic volcanic rocks of Saudi Arabia.Saudi Arabian Deputy Ministry for Mineral Resources Open-File Report USGS-OF-03093,82p.
Clague, D. and Ferry, F., 1982: Petrology and Trace Elements Geochemistry of Honolulu Volcanism: Implication for the Ocean Mantle below Hawaii. Journal of Petrology,V.23, pp.447-504.
Cox, K., Bell, J. and Pankhurst, R., 1979: The Interpretation of Igneous Rocks. Springer, London.
Downes, H., Seghed, I., Szakacs, A., Dobasi, G., James, D., Vaselli, O., Rigby, I., Ingram, G., Rex, D. and Peckskay, Z., 1995: Petrology and Geochemistry of Late Tertiary-Quaternary Mafic Alkali Volcanism in Romania. Lithos, V.35,pp.65-81.
Duffield, W., Edwin, A., Mckee, H., Salem, F.and Teimeh, M., 1987: K-AR ages, Chemical Composition And Geothermal significance of Cenozoic Basalt near the Jordan Rift. Technical report. NRA, Amman.
El- Akhal, H., 2004: Contribution to the petrography, geochemistry, and tectonic setting of the basalt flows of the Umm-Qais plateau, north Jordan. Geological Bulletin of Turkey, V .47, pp.1-12.
El-Hasan, T. and Al-Malabeh, A., 2008: Geochemistry, Mineralogy and Petrogenesis of El-Lajjoun Pleistocene Alkali Basalt of Central Jordan. Jordan Journal of Earth and Environmental Sciences, V.1, pp.53-62.
Frey, F. A., Green, D. H. and Roy, S. D.,1978: Integrated Models of Basalt Petrogenesis: A Study of Quartz The oliites to Olivine Melilites from South Eastern AustraliaUtilizing Geochemical and Experimental Petrological Data. Journal of Petrology, V.19, pp.463-513.
George, S., John, M., Costas, X. and Gavin, H., 2010: Petrogenesis of Latest Miocene-Quaternary Continental Intraplate Volcanism along the Northern Dead Sea Fault System (Al-Ghab-Homs Volcanic Field), Western Syria: Evidence for Lithosphere-Asthenoshere Interaction. Journal of Petrology, pp.1-30.
Ghent, E. D., Coleman, R. G., and Hadley, D. G., 1980: Ultramafic inclusion and host alkali olivine basalts of southern coastal plain of the Red Sea. Saudi Arabia. Amer. J. Sci, pp. 280-284, pp. 499-527.
Gregory, R. T., Coleman R. G., and Brown, G. F., 1982: Cenozoic volcanic rocks of Saudi Arabia. Evidence from continent for two stages of opening of the Red Sea. Geol. Sci. Am. Prog., V. 14(7). pp.502.
Guba. I and Mustafa. H., 1988: Structural Control of Young Basaltic Fissure Eruptionin the Plateau Basalt Area of the Arabian Plate, Northeastern Jordan, Journal of Volcanology and Geothermal Research, pp.319-334.
Hollocher, K.,2004:CIPW Norm Calculation Program. Geology Department, Union College.
Ibrahim, K. M., Tarawneh, K., Rabbaa, I., 2003: Phases of activity and geochemistry of basaltic dike systems in northeast Jordan parallel to the Red Sea. J. Asian EarthSci. V.21, pp. 467–472.
Ibrahim, K. M., 1993: The geological framework for the Harrat Ash Shaam Basaltic Super-Group and its volcanic evolution. NRA, Geological Mapping Division Bulletin 25, pp.33.
Ilani, S., Harlavan, Y., Tarawneh, K., Rabba, I., Weinberger, R., Ibrahim, K., Peltz, S. and Steinitz, G., 2001: NewK-ArAgesof Basalts from the Harrat Asham Volcanic Field in Jordan: Implications for the Span and Duration of Upper Mantle Upwelling Beneath the Western Arabian Plate. Geology, V.29, pp. 171-174.<0171:NKAAOB>2.0.CO;2
Israa S. Abu-Mahfouz, Ahmad A. Al-Malabeh and Shaher M.Rababeh, 2016:Geo-engineering evaluation of Harrat Irbid Basaltic Rocks, Irbid District—North Jordan, Arab J.Geosci. V.9: pp.412-421; DOI10.1007/s12517-016-2428-4
Kerr, P., 1977:Optical Mineralogy .John Wiley and Sons, New York.
Jenner, G.,Gawood, P., Rautenschlein, M. and White, W., 1987: Composition of Back-Arc Basin Volcanic Valufa Ridge Lau Basin: Evidence for a Slab-Derived Component in Their Mantle Source. Journal of Volcanology and Geothermal Research,V.32,pp.209-222.
Le Maitre, R. W., Bateman, P.,Dudek, A., Keller,J.,Lameyre Le Bas, M. J., Sabine, P. A.,Schmid, R., Sorensen, H., Streckeisen, A., Woolley, A. R. and Zanettin, B., 1989: A Classification of Igneous Rocks and Glossary of Terms. Black well, Oxford.
Mackenzie, W. S., Donaldson, C. H., Guilford, C., 1982: Atlas of igneous rock and their textures. England: Longman Scientific and Technical.
Ma, G. S.-K., Malpas, J., Xenophontos, C. and Chan, G. H.-N., 2011: Petrogenesis of Latest Miocene-Quaternary Continental Intraplate Volcanism along the Northern Dead Sea Fault System (Al-Ghab-Homs Volcanic Field), Western Syria: Evidence for Lithosphere-Asthenoshere Interaction. Journal of Petrology, pp.1-30.
Middelmost, E., 1975: The Basalt Clan. Earth-Science Reviews, V.11, pp.337-564.
Moffat D. T., 1988: A Volcaotectonic Analysis of the Ceno-zoic Continental Basalts of Northern Jordan; Implications for Hydrocarbon Prospecting in the Block.B Area.Unpubl. Report. University college of Swansen, Uk.
Moghazi, A. M., 2003: Geochemistry and Petrogenesis of a High-KCalc-Alkaline Dokhan Volcanic Suite, South Safaga Area, Egypt: The Role of Late Neoproterozoic Crustal Extension. Precambrian Research, V.125, pp.161-178.
Mor, D. and Steinitz, G., 1985: The history of the Yarmouk River based on K-Ar dating and its implication on the development of the Jordan rift. Isr. Geol. Surv. Rep. GSI/40/85,pp.18,Jerusalem.
Norry, M. J. and Fitton, J. G., 1993: Compositional Differences between Oceanic and Continental Basic Lavas and Their Significance. In: Hawkes worth, C. J. and Norry, M. J.,Eds., Continental Basalts and Mantle Xenoliths, Shiva Publishing Ltd., Cheshire, pp. 5-19
Pearce, J. A. and Cann, J. R., 1973: Tectonic Setting of Basic Volcanic Rocks Determined Using Trace Element Analyses. Earth and Planetary Science Letters, V. 19, pp.290-300.
Pearce T. H., Gorman, B. E. and Birkett, T. C., 1977: The Relationship between Major Element Chemistry and Tectonic Environment of Basic and Intermediate Volcanic Rocks. Earth and Planetary Science Letters, V.36, pp.121-132. (77)90193-5.
Pearce J. A., 1983: Role of the sub-continental lithosphere in magma genesis at active continental margins. In: Hawkes worth C. J. and Norry M. J, (eds), Continental basalts and mantle xenoliths. Shiva, Nantwich, pp. 230-249.
Pearce, J., Harris, N. and Tindle, A., 1984:Trace Element Discrimination Diagram for the Tectonic Interpretation of Granitic Rocks. Journal of Petrology, V.25, pp.956-983.
Peltz, S. and Bratosia W., 1986: New Data on the Geochemistry of the Quaternary Basalts in Pensani Mountains. Geophics, V.71, pp. 389-403
Ponicarov, V .P., Kazmin, V. G., Mikhailov, LA., Razvaliayev, A. V., Krasheninnikov, A. V., Kozlov, V. V., Souiidi-Kondratiyev, E. D., Mikhailov, K. YA., Kulakov,V. V., Faradzhev, V. A., Mirzayev, K. M.,1967: The geology of Syria.Explanatory Notes of the geological map of Syria, Part1.Dept.of Geological and Mineral Research. S.A.R.
Rollinson, H. R., 1993: Using Geochemical Data: Evaluation, Presentation, Interpretation. Longman Scientificand Technical, England. p.352.
Shaw, J. E., Baker, J. A., Menzies, M. A., Thirlwall, M. F. and Ibrahim, K. M., 2003: Petrogenesis of the Largest Intraplate Volcanic Field on the Arabian Plate (Jordan):A Mixed Lithosphere-Asthenosphere Source Activated by Lithospheric Extension. Journal of Petrology, V.44, pp.1657-1679.
Shaw, J. (2003): Geochemistry of Cenozoic Volcanism and Arabian Lithospheric Mantle in Jordan. Unpublished PhD. Thesis, University of London, London.
Smadi Ali K, (2016): Mineralogy, Geochemistry and petrogensis of selected basaltic outcrops in central parts of Irbid Governorate, North Jordan. Master of Science in Geology Thesis, Yarmouk University, Irbid Jordan, pp.137.
Steinitz, G. and Baratov, Y., 1992: The Miocene-Pleistocene history of the Dead Sea Segment of the Rift in Light or K-Ar Age of Basalts. Israel Journal of Earth Sciences, V.40, pp.199-208.
Sun, S. S. and Mac Donough, W. F., 1989: Chemicaland Isotopic Systematic of Oceanic Basalts Implications for Mantle Composition and Processes in Magmatism in the Ocean Basins. Geological Society, London, Special Publication, V. 42, pp. 313-345.
Tarawneh K, S. Ilani, I. Rabba, Y. Harlavan, S. Peltz, K. Ibrahim, R. Weinberger and G. Steinitz, 2000: Dating of the Harat Ash Shaam Basalt Northeast Jordan. Report GSI/2/2000: Jordan, Natural Resources Authority (NRA), and Geological Survey of Israel, Jerusalem.
Thompson, R. N., 1987: Phase Equilibria Constraints on the Genesis and Magmatic Evolution of Oceanic Basalts. Earth Science Reviews, V.24, pp. 161-210.
Wilson, M., 1989: Igneous Petrogenesis. Un win Hyman Ltd., London, pp. 466.
Winter, J. D. 2001: An Introduction to Igneous and Metamorphic Petrology. Prentice HallInc., Upper Saddle River, pp.697.
Wiesemann, G., Abdullatif, A., 1963: Geology of The Yarmouk Area, North Jordan. Un publ. Rept. With 10 Petrography, Geochemistry, and Tectonic Setting, North Jordan geol. maps, scale1:10,000. Fe d. Inst.of Geosc. And Nat. Res., Hannover; nat.res. au th., Amman.
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