Zobrazeno 1 - 9
of 9
pro vyhledávání: '"A. L. Grokholsky"'
Autor:
E. P. Dubinin, A. L. Grokholsky
Publikováno v:
Геодинамика и тектонофизика, Vol 11, Iss 3, Pp 522-547 (2020)
The study was focused on the tectonic structure features of the Gulf of Aden, which includes three provinces. The western, central and eastern provinces differ in morphostructural segmentation of the spreading ridge of the Gulf of Aden, which took pl
Externí odkaz:
https://doaj.org/article/4a78c0476e4b41fa89f7990947741462
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :19-27
The problem of the interaction of spreading ridges with large igneous provinces is widely discussed in the scientific literature. The most striking and well-preserved example of such interaction in the geological past is the “collision” of the So
Publikováno v:
Moscow University Geology Bulletin. 77:633-640
Autor:
Anastasia I. Chupakhina, Evgeny P. Dubinin, Andrey L. Grokholsky, Darya A. Ryzhova, Andrey A. Bulychev
Publikováno v:
Вестник ВГУ Серия Геология. :89-98
Publikováno v:
Oceanology. 61:543-554
The features of structure formation on the adjacent margins of Iberia and Newfoundland are considered based on an analysis of geological and geophysical data and physical modeling. These margins represent the passive margins formed during hyperextens
Publikováno v:
Физика Земли. :76-91
The paper addresses crustal formation in the Australian–Antarctic basin at the early period of separation of Australia and Antarctica. The study covers long rifting (~160–80 Ma), ultraslow spreading (~80–45 Ma) with the formation of proto-ocean
Publikováno v:
Geotectonics. 48:87-103
The off-axis topography of spreading ridges is a result of tectonic and magmatic processes occurring in the axial zone and operating off the ridge axis during further evolution of the crust. The results of physical and numerical simulations have show
Publikováno v:
Oceanology. 52:688-699
The rift zone’s relief, the spreading kinematics, and the experimental modeling of the Knipovich Ridge’s formation were analyzed. Its rift zone is formed in a transtension environment. Faulting is predominant in its northern part, while strike-sl
Publikováno v:
Tectonophysics. 199:389-404
Physical modelling and geodynamic analysis have been carried out concerning the formation and evolution of overlapping spreading centers (OSCs) with fast spreading rates. Crust and underlying magma chamber were modelled by (solidified and melted resp