Evidence for Paleocene–Eocene evolution of the foot of the Eurasian margin (Kermanshah ophiolite, SW Iran) from back-arc to arc: Implications for regional geodynamics and obduction H. Whitechurch
The Kermanshah ophiolites (KO) crop out along the Main Zagros Thrust and consist of an ophiolitic mé...
The Late Cretaceous–early Paleogene tectonic evolution of the Iranian Plateau is not well understood...
New trace-element, radiogenic Sr-Nd-Pb isotopic and geochronological data from Middle-Late Cretaceou...
International audienceThe nature and significance of the Kermanshah ophiolite (Zagros Mountains, Ira...
International audienceThe nature and significance of the Kermanshah ophiolite (Zagros, Iran), classi...
Iran is a mosaic of continental terranes of Cadomian (520-600 Ma) age, stitched together along sutur...
International audiencehe Khoy region (NW Iran) is important in the clarification of the structural f...
The Zagros fold-and-thrust belt of SW Iran is a young continental convergence zone, extending NW–SE ...
Late Cretaceous Neyriz ophiolite, as a part of the Outer Zagros Ophiolitic Belt, represents a remnan...
Onset timing in the Zagros collisional belt is critically important for understanding the early hist...
Iran is a mosaic of Ediacaran-Cambrian (Cadomian; 520-600. Ma) blocks, stitched together by Paleozoi...
New and compiled geochemical, isotopic and geochronological data allow us to propose a new explanati...
New and compiled geochemical, isotopic and geochronological data allow us to propose a new explanati...
Second Arabian Plate Geology Workshop Abu Dhabi, UAE, 24 - 27 January 2010The emplacement of ophioli...
A poorly understood lag time of 15-20 m.y. exists between the initial Arabia-Eurasia continental col...
The Kermanshah ophiolites (KO) crop out along the Main Zagros Thrust and consist of an ophiolitic mé...
The Late Cretaceous–early Paleogene tectonic evolution of the Iranian Plateau is not well understood...
New trace-element, radiogenic Sr-Nd-Pb isotopic and geochronological data from Middle-Late Cretaceou...
International audienceThe nature and significance of the Kermanshah ophiolite (Zagros Mountains, Ira...
International audienceThe nature and significance of the Kermanshah ophiolite (Zagros, Iran), classi...
Iran is a mosaic of continental terranes of Cadomian (520-600 Ma) age, stitched together along sutur...
International audiencehe Khoy region (NW Iran) is important in the clarification of the structural f...
The Zagros fold-and-thrust belt of SW Iran is a young continental convergence zone, extending NW–SE ...
Late Cretaceous Neyriz ophiolite, as a part of the Outer Zagros Ophiolitic Belt, represents a remnan...
Onset timing in the Zagros collisional belt is critically important for understanding the early hist...
Iran is a mosaic of Ediacaran-Cambrian (Cadomian; 520-600. Ma) blocks, stitched together by Paleozoi...
New and compiled geochemical, isotopic and geochronological data allow us to propose a new explanati...
New and compiled geochemical, isotopic and geochronological data allow us to propose a new explanati...
Second Arabian Plate Geology Workshop Abu Dhabi, UAE, 24 - 27 January 2010The emplacement of ophioli...
A poorly understood lag time of 15-20 m.y. exists between the initial Arabia-Eurasia continental col...
The Kermanshah ophiolites (KO) crop out along the Main Zagros Thrust and consist of an ophiolitic mé...
The Late Cretaceous–early Paleogene tectonic evolution of the Iranian Plateau is not well understood...
New trace-element, radiogenic Sr-Nd-Pb isotopic and geochronological data from Middle-Late Cretaceou...