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Titlebook: Arabian Plate and Surroundings:Geology, Sedimentary Basins and Georesources; Sami Khomsi,François M. Roure,Ammar Amin Book 2020 Springer N

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https://doi.org/10.1007/978-3-663-07212-6tics, with striation showing a multiphase history. During Mesozoic times, the extensional activity of WNW- to- NW-trending normal faults is associated with significant thickness and/or facies variations comprising abundant syntectonic sequences. The growth of major synsedimentary typical normal faul
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Stress Erythropoiesis Model Systems,most mantle <80 km deep in an intra-oceanic island arc. This suggests that the mafic intrusive rocks of Bulghah and Humaymah represent the plutonic equivalents of the Arabian Shield arc metavolcanic calc-alkaline rocks. The compositional variations from granodiorite to monzogranite of Bulghah and Hu
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Theodosia Kalfa,Kathleen E. McGrath.27 with average of about 0.16, indicating that the common structure types is a contact (fault) model. Magnitude magnetic transforms is used it demonstrate the subsurface features where it is compared with the conventional reduce to pole technique to extra the zones if any. Also, this technique used
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