Some of the most important, rapid, and enigmatic changes in our Earth's environment and
biota occurred during the Neoproterozoic Era (1000–540 million years ago; Ma). Paramount …

During the late Cryogenian–Ediacaran (650–542Ma), the Arabian–Nubian Shield (ANS)
underwent final assembly and accretion to the Saharan Metacraton concurrent with the …

Comparative geology suggests that the continents adjacent to northern, western, southern,
and eastern Laurentia in the Late Proterozoic were Siberia, Australia-Antarctica, southern …

The assembly of the eastern part of Gondwana (eastern Africa, Arabian–Nubian shield
(ANS), Seychelles, India, Madagascar, Sri Lanka, East Antarctica and Australia) resulted …

We here summarize the evolution of the greater Red Sea–Gulf of Aden rift system, which
includes the Gulfs of Suez and Aqaba, the Red Sea and Gulf of Aden marine basins and …

The Zagros fold-thrust belt in Iran forms the external part of the Zagros active orogenic
wedge. It includes a sequence of heterogeneous latest Neoproterozoic–Phanerozoic …

The Arabian Plate originated∼ 25Ma ago by rifting of NE Africa to form the Gulf of Aden and
Red Sea. It is one of the smaller and younger of the Earth's lithospheric plates. The upper …

▪ Abstract Turkic-type orogeny is a class of collisional mountain building, in which the
precollision history of one, or both, of the colliding continents involves the growth of very …

The Paleozoic section became prospective during the early 1970s when the enormous gas
reserves in the Permian Khuff reservoirs were delineated in the Gulf and Zagros regions and …

The magmatic and tectonic history of the Yangtze Block and its possible affinity with other
Neoproterozoic arc terranes are important elements in the reconstruction of Neoproterozoic …