Sedimentology of Sinjar Limestone Formation, Sulaimanian area, Northeastern Iraq
Sinjar Limestone Formation of Eocene age is composed of allochthonous and autochthonous limestones. Petrographic and geochemical characteristics of the rocks of this Formation show the occurrence of phosphatic rocks in two horizons which are separated by 43 feet thick nonphosphatic limestone beds. T...
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Dokumentumtípus: | Cikk |
Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1985
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Sorozat: | Acta mineralogica-petrographica
27 |
Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
Tárgyszavak: | |
Online Access: | http://acta.bibl.u-szeged.hu/24731 |
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005 | 20220726110038.0 | ||
008 | 161017s1985 hu o 0|| eng d | ||
022 | |a 0365-8066 | ||
040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
041 | |a eng | ||
100 | 1 | |a Mallick Khalil Ahmed | |
245 | 1 | 0 | |a Sedimentology of Sinjar Limestone Formation, Sulaimanian area, Northeastern Iraq |h [elektronikus dokumentum] / |c Mallick Khalil Ahmed |
260 | |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology |b Szeged |c 1985 | ||
300 | |a 101-116 | ||
490 | 0 | |a Acta mineralogica-petrographica |v 27 | |
520 | 3 | |a Sinjar Limestone Formation of Eocene age is composed of allochthonous and autochthonous limestones. Petrographic and geochemical characteristics of the rocks of this Formation show the occurrence of phosphatic rocks in two horizons which are separated by 43 feet thick nonphosphatic limestone beds. The study also reveals that the phosphatic rocks are recycled sedimentary deposits from the near-by source. No effects of phosphatization was observed in the associated rocks. Five phases of sedimentation representing different physicochemical controls have been established on the basis of petrography, chemistry and the fossils present in them. | |
650 | 4 | |a Természettudományok | |
650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
695 | |a Kőzettan, Ásványtan, Földtan | ||
700 | 0 | 2 | |a Al-Qayem Basim J. |e aut |
856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/24731/1/mineralogica_027_101-116.pdf |z Dokumentum-elérés |