Mineralogy, petrology and Geochemistry of the Basalt flows at Ash-Shun Ash-Shamaliyya Area, North West Jordan

Ibrahim Ahmad Ali Bany Yaseen; Alaa Yaser Abidrabbu

doi:doi:10.11648/j.earth.20160506.11

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Mineralogy, petrology and Geochemistry of the Basalt flows at Ash-Shun Ash-Shamaliyya Area, North West Jordan

Ibrahim Ahmad Ali Bany Yaseen, Alaa Yaser Abidrabbu

Received: 29 August 2016 Accepted: 5 October 2016 Published: 7 November 2016

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Abstract

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.

DOI	10.11648/j.earth.20160506.11
Published in	Earth Sciences (Volume 5, Issue 6, December 2016)
Page(s)	82-95
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Calc-Alkaline Basalt, Tectonic Setting, Fractionation, Ash-Shuna Ash-Shamaliyya, Jordan

References

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Ibrahim Ahmad Ali Bany Yaseen, Alaa Yaser Abidrabbu. (2016). Mineralogy, petrology and Geochemistry of the Basalt flows at Ash-Shun Ash-Shamaliyya Area, North West Jordan. Earth Sciences, 5(6), 82-95. https://doi.org/10.11648/j.earth.20160506.11

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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 Sci. 2016, 5(6), 82-95. doi: 10.11648/j.earth.20160506.11

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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 Sci. 2016;5(6):82-95. doi: 10.11648/j.earth.20160506.11

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@article{10.11648/j.earth.20160506.11,
  author = {Ibrahim Ahmad Ali Bany Yaseen and Alaa Yaser Abidrabbu},
  title = {Mineralogy, petrology and Geochemistry of the Basalt flows at Ash-Shun Ash-Shamaliyya Area, North West Jordan},
  journal = {Earth Sciences},
  volume = {5},
  number = {6},
  pages = {82-95},
  doi = {10.11648/j.earth.20160506.11},
  url = {https://doi.org/10.11648/j.earth.20160506.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20160506.11},
  abstract = {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.},
 year = {2016}
}

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TY  - JOUR
T1  - Mineralogy, petrology and Geochemistry of the Basalt flows at Ash-Shun Ash-Shamaliyya Area, North West Jordan
AU  - Ibrahim Ahmad Ali Bany Yaseen
AU  - Alaa Yaser Abidrabbu
Y1  - 2016/11/07
PY  - 2016
N1  - https://doi.org/10.11648/j.earth.20160506.11
DO  - 10.11648/j.earth.20160506.11
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 82
EP  - 95
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20160506.11
AB  - 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.
VL  - 5
IS  - 6
ER  -

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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

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Ibrahim Ahmad Ali Bany Yaseen, Alaa Yaser Abidrabbu. (2016). Mineralogy, petrology and Geochemistry of the Basalt flows at Ash-Shun Ash-Shamaliyya Area, North West Jordan. Earth Sciences, 5(6), 82-95. https://doi.org/10.11648/j.earth.20160506.11

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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 Sci. 2016, 5(6), 82-95. doi: 10.11648/j.earth.20160506.11

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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 Sci. 2016;5(6):82-95. doi: 10.11648/j.earth.20160506.11

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@article{10.11648/j.earth.20160506.11,
  author = {Ibrahim Ahmad Ali Bany Yaseen and Alaa Yaser Abidrabbu},
  title = {Mineralogy, petrology and Geochemistry of the Basalt flows at Ash-Shun Ash-Shamaliyya Area, North West Jordan},
  journal = {Earth Sciences},
  volume = {5},
  number = {6},
  pages = {82-95},
  doi = {10.11648/j.earth.20160506.11},
  url = {https://doi.org/10.11648/j.earth.20160506.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20160506.11},
  abstract = {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.},
 year = {2016}
}

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TY  - JOUR
T1  - Mineralogy, petrology and Geochemistry of the Basalt flows at Ash-Shun Ash-Shamaliyya Area, North West Jordan
AU  - Ibrahim Ahmad Ali Bany Yaseen
AU  - Alaa Yaser Abidrabbu
Y1  - 2016/11/07
PY  - 2016
N1  - https://doi.org/10.11648/j.earth.20160506.11
DO  - 10.11648/j.earth.20160506.11
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 82
EP  - 95
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20160506.11
AB  - 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.
VL  - 5
IS  - 6
ER  -

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