Titlebook: Lithosphere Dynamics and Sedimentary Basins: The Arabian Plate and Analogues; Khalid Al Hosani,Francois Roure,Stephen Lokier Conference pr

fatty-streak

Architecture of the Oman–UAE Ophiolite: Evidence for a Multi-Phase Magmatic Historyences to normal midocean ridge basalt (MORB). Mineral and whole-rock geochemical analyses show that the early crustal rocks are chemically similar to MORB, but the later magmatic sequence has chemical features typically found in suprasubduction zone (SSZ) settings. The ophiolite in the United Arab E

裂隙

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The Jurassic–Cretaceous depositional and tectonic evolution of the southernwestern margin of the Neon to be established. The model charts the progressive breakup of the Arabian continental margin and closure of Neotethys during the mid to late Cretaceous and is divided into three main stages: Stage 1—Initial rifting and formation of the Neotethys Ocean, followed by a prolonged period of stable, pa

Indurate

Forced Folding of the Neoautochthonous Late Cretaceous–Early Tertiary Sequence at the Western End ofain’ folds and NE–SW-trending ‘Cross’ folds superimposed on them. These folds appear to be dominantly forced folds that developed as a result of repeated uplift and depression of basement blocks. Their trends correspond to the trends of the subjacent basement blocks. Hence, the Jebel Rawdha folds tr

Esophagitis

Seismic stratigraphy and subsidence history of the United Arab Emirates (UAE) rifted margin and overisodes of rifting punctuated by periods of relative tectonic quiescence and thermal subsidence. An initial age of rifting of 260 Ma and a stretching factor, ., of 1.2 was followed by second period of stretching with an initial age of rifting of 180 Ma, and ., of 1.1. This model accounts for the gene

syring

Depth seismic imaging using reflection and first arrival traveltime tomography: Application to a deeal foothills part of the profile, the velocity model was computed by joint inversion using the first arrivals down to 4 km depth and the reflected travel times for deeper layers. In the eastern part of the profile, due to the outcropping of the Semail ophiolite, the deep reflection events are not vi

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LUCY

Interstellar

Diagenesis of the Khuff Formation (Permian–Triassic), Northern United Arab Emiratesion of carbonate sediments by modified marine pore waters; (2) formation of coarsecrystalline dolomite cement by highly evolved marine pore waters (13–23 wt% NaCl eq.) at elevated temperatures (120–208 °C), and (3) calcite cementation by highly saline fluid (20–23 wt% NaCl eq.) at high temperature (

ABHOR

Evidence for Mantle Exhumation Along the Arabian Margin in the Zagros (Kermanshah Area, Iran)ment has been identified further to the NE on Eocene gabbro. So far, this one is considered as an intra-oceanic detachment from the residual Tethys. A first evolution model is proposed from early Jurassic to late Cretaceous obduction along with how this interpretation may be improved by future field