The Qom Formation is the most important hydrocarbon reservoir target in Central Iran.The Qom platform developed in a back-arc basin during the Oligo-Miocene due to the closing of the Tethyan Seaway.This formation cons...
This work was supported by a National Natural Science Foundation of China(Grant No.91958210);the Government Finance Level II Project(No.DD20190083);‘the 13th Five-Year Plan’National Science and Technology Major Project(No.2016ZX05034001-003).
The late Permian(Lopingian)was a crucial climate transition period from the late Paleozoic Ice Age to the early Triassic of exceptionally high temperatures.However,the origins of the third-order sea-level changes duri...
Observational facts from the Maldives, Goa and Bangladesh in the Indian Ocean and from Fiji and New Caledonia in the Pacific record a high sea level in the 17th century, a low sea level in the 18th century, a high sea...
Global sea level has today become widely understood merely in terms of glacial eustasy and thermal expansion. Although this is good in theory, it is not enough to explain observational facts in nature. We know that th...
the German Academic Exchange Service(DAAD);the Egyptian Ministry of Higher Education and Scientific Research(the "GERLS" Programme) for their financial support
The Jurassic succession at Gebet Maghara, North Sinai, Egypt, represents a mixed carbonate-siticictastic sequence. Combining information from both fossits and rocks attowed a ptausibte reconstruction of the deposition...
This study was jointly supported by the national research project "sequence stratigraphy of ancient continent and peripheral areas and change of sea level in East China" and the doctoral station of sedimentology at University of Petroleum,Beijing.
In light of the principle of sequence stratigraphy, detailed analysis of depositionalsequences and systematical carbon isotope measurements were done for the Triticites zone ofthe typical Late Carboniferous section in...
During Permian and Triassic the western margin of Upper Yangtze platform had experienced an evolution from early rift stage to thermal subsidence and then to foreland basin. The tectonic transformations have resulted...
The rupture of the lithosphere in Late Jurassic brought about the eruption of basaltic magma in the Songliao Basin. The evolution of the basin in Cretaceous progressed through six stages: pre-rift doming, extensional ...
Since Mrner presented his geoidal eustatic change theory in 1976, attention has been paid to the effects of geoid changes on sea level, but up to now no one has discussed the geoid changes and geoidal eustasy in China...