This book investigates the late Neoproterozoic N-S trending Wadi Yiba Shear Zone (WYSZ) in southern Arabian Shield. WYSZ played a significant role in the structural shaping of the basement lithologies (gneisses, metavolcanics, Ablah Group (meta-clastic and marble units) and syn- and post-tectonic granitoids) exposed in Wadi Yiba, Asir tectonic terrane. Effects of, at least, three phases of deformation are detected (D1–D3). Among these phases, D2 deformation phase was intensive and pervasive, and responsible for the formation of the WYSZ. Minor and major F2 thrust- and shear zone-related folds are coeval to this phase. The deformation patterns in the area reflect the progressive convergence between East and West Gondwanalands
Les informations fournies dans la section « Synopsis » peuvent faire référence à une autre édition de ce titre.
This book investigates the late Neoproterozoic N-S trending Wadi Yiba Shear Zone (WYSZ) in southern Arabian Shield. WYSZ played a significant role in the structural shaping of the basement lithologies (gneisses, metavolcanics, Ablah Group (meta-clastic and marble units) and syn- and post-tectonic granitoids) exposed in Wadi Yiba, Asir tectonic terrane. Effects of, at least, three phases of deformation are detected (D1–D3). Among these phases, D2 deformation phase was intensive and pervasive, and responsible for the formation of the WYSZ. Minor and major F2 thrust- and shear zone-related folds are coeval to this phase. The deformation patterns in the area reflect the progressive convergence between East and West Gondwanalands
Ghazi Kattu; Senior Geologist, M.Sc., Saudi Geological Survey (SGS).Prof. Zakaria Hamimi; Prof. of Structural Geology, King Abdulaziz University, Saudi Arabia.Dr. Mohamed El-Shafei; Assoc. Prof. of Structural Geology, King Abdulaziz University, Saudi Arabia.
Les informations fournies dans la section « A propos du livre » peuvent faire référence à une autre édition de ce titre.
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