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Regularities and geohistorical prerequisites of oil and gas specializationof rift sedimentary basins of AfricaSedimentary basins of Late Phanerozoic rift origin are locatedin Africa and on its underwater
Developing the Cambrian and Ordovician Magnetic Polarity Time Scale: Current Data and Attempt of Synthesis for the Cenozoic, Mesozoic, and Late Paleozoic. However, our understanding of the behavior of geomagnetic polarity
Rift Margination and Destroing of Africa Late Phanerozoic rifts were related to ancient lateral heterogeneity of the consolidated crust.
Rift and epirift structures of North-East Vietnam and their probable analoguesIn the north-western region of Vietnam riftogenesis processes occurred in Phanerozoic in a single
Global latitudinal lineament system and its possible origin of dominate meridional extended and compressed Phanerozoic and Late Proterozoic belts can be related
Southwestern Gondwana's Permian climate amelioration recorded in coal-bearing deposits of the Moatize sub-basin (Mozambique) The postglacial climate history of Gondwana represents the most prominent climate amelioration in the Phanerozoic
Structural analysis and paleostress evolution in the Imiter silver mining region, Eastern Anti Atlas, Morocco: Implications for mineral exploration the Phanerozoic. In this investigation, a structural analysis of the different geological units revealed multi
Systematics of Early Cambrian Paleomagnetic Directions from the Northern and Eastern Regions of the Siberian Platform and the Problem of an Anomalous Geomagnetic Field in the Time Vicinity of the Proterozoic–Phanerozoic Boundary history shows that the peculiarities observed in Siberia in the paleomagnetic record for the Precambrian–Phanerozoic
Paleoenvironments and age of the Talampaya Formation: The Permo-Triassic boundary in northwestern Argentina, at least in this locality, sedimentation occurred during the Late Permian but may have extended
The First Data on the N Isotopic Composition of the Permian and Triassic of Northeastern Russia and Their Significance for Paleotemperature Reconstructions in the Late Wuchiapingian and Early Changhsingian (Late Permian) changed in the Boreal Superrealm to less
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