Zobrazeno 1 - 6
of 6
pro vyhledávání: '"G. D. Agranov"'
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d86e4510062062ffa77ce7da82e08148
https://doi.org/10.33623/0579-9406-2022-5-19-27
https://doi.org/10.33623/0579-9406-2022-5-19-27
Publikováno v:
Moscow University Geology Bulletin. 77:633-640
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::69dfc7780bcf49604d9caf976e419ce6
https://doi.org/10.3103/s0145875222060035
https://doi.org/10.3103/s0145875222060035
Publikováno v:
Lithology and Mineral Resources. 57:380-391
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::208ec132187d52c54fd1cf42d27866ef
https://doi.org/10.1134/s0024490222050078
https://doi.org/10.1134/s0024490222050078
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7d73c7a153e24d91243654d413ebd00c
https://doi.org/10.31857/s0002-33372019276-91
https://doi.org/10.31857/s0002-33372019276-91
Publikováno v:
Izvestiya, Physics of the Solid Earth. 55:256-269
The peculiarities of the formation of the structure of the Earth’s crust in the Australian–Antarctic basin during the early break-up between Australia and Antarctica are considered. The study period encompasses long-lasting rifting (~160–80 Ma)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1fab02f75ac5d538b8c27567e46c64b4
https://doi.org/10.1134/s1069351319020022
https://doi.org/10.1134/s1069351319020022
Publikováno v:
Geotectonics. 52:499-515
The paper considers geological and geophysical data on the crustal structure of the volcanic Kerguelen Plateau and nearby Indian Ocean, as well as evolution of the Kerguelen Plateau during the Gondwana breakup. It is assumed that three isolated conti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61ced0dc2af8c5a4c72faae5c8b19d43
https://doi.org/10.1134/s0016852118050035
https://doi.org/10.1134/s0016852118050035