Zobrazeno 1 - 10
of 16
pro vyhledávání: '"M. N. Shapiro"'
Publikováno v:
Russian Journal of Earth Sciences. 12:1-13
The collision of the Cretaceous Olutorsky Island Arc with eastern Eurasia margin in the northwest Pacific is a critical event in Cenozoic evolution of the Pacific Rim. The timing of synorogenic flysch deposition (Paleocene–Middle Eocene, as young a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cfbca6dc9cb4b1319082b8200889087f
https://doi.org/10.2205/2011es000504
https://doi.org/10.2205/2011es000504
Autor:
A. V. Solov’ev, M. N. Shapiro
Publikováno v:
Geotectonics. 45:210-224
Two belts of subaerial volcanic rocks—the Eocene Kinkil belt and the Neogene belt of the Sredinny Range—extend along the Kamchatka Isthmus. It is suggested that their formation is related to subduction of the oceanic lithosphere beneath the conti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f11a47e22e5b39740967c05f521ae7b9
https://doi.org/10.1134/s0016852111030071
https://doi.org/10.1134/s0016852111030071
Publikováno v:
Geotectonics. 42:469-487
The lateral variability of structural elements in the collision zone of the Cretaceous-Paleocene Achaivayam-Valagin island arc with the northeastern Asian margin is considered. The similarity and difference of Eocene collision structural elements in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dc813b3a6b4ba8ba3637e0f0ac474f2a
https://doi.org/10.1134/s0016852108060046
https://doi.org/10.1134/s0016852108060046
Autor:
A. V. Solov’ev, John I. Garver, Sarah A. Johnston, D. M. Ol’shanetskii, M. N. Shapiro, T. N. Palechek
Publikováno v:
Stratigraphy and Geological Correlation. 15:112-119
In the Sredinnyi Range of Kamchatka, the Baraba Formation of continental conglomerates is assumed to be of the late Campanian age based on found flora remains, but data of isotopic geochronology suggest the Eocene age of these deposits. New data on r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::45c45fc58c10e6e7591c4d9c46f7eef4
https://doi.org/10.1134/s0869593807010091
https://doi.org/10.1134/s0869593807010091
Autor:
M. Yu. Khotin, M. N. Shapiro
Publikováno v:
Geotectonics. 40:297-320
Ophiolites of the Afrika Mys Block of the Kamchatsky Mys Peninsula, eastern Kamchatka, are a fragment of an accretionary prism that formed in the Late Cretaceous-Eocene on the southern side of the Kronotsky island arc as a result of its collision wit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ab3c08a85528d0c810a2971db6252b1
https://doi.org/10.1134/s0016852106040042
https://doi.org/10.1134/s0016852106040042
Publikováno v:
Russian Journal of Earth Sciences. 6:105-132
The provenance and tectonic setting of the sediments and rare cobbles from the accretionary wedge on Karaginski Island were examined. This study provides a picture of the nature of the NE Asian paleomargin in the middle Eocene to early Miocene. The t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::25bc56b602d356cbb69c337c03715169
https://doi.org/10.2205/2004es000152
https://doi.org/10.2205/2004es000152
Autor:
John I. Garver, Igor R. Kravchenko-Berezhnoy, Alexei V. Soloviev, M. N. Shapiro, E. A. Shcherbinina
Publikováno v:
The Island Arc. 11:79-90
The Lesnaya Group is part of a thick, poorly dated turbidite assemblage that sits in the footwall of a regionally extensive collision zone in which the Cretaceous–Paleocene Olutorsky island arc terrane was obducted onto continental margin basin str
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c8ee22ef5119defc9f806d8b8438ef95
https://doi.org/10.1046/j.1440-1738.2002.00353.x
https://doi.org/10.1046/j.1440-1738.2002.00353.x
Publikováno v:
Lithology and Mineral Resources. 36:322-336
The mineral composition of sandstones from Cretaceous-Lower Paleocene terrigenous sequences of the western Kamchatka-Ukelayat zone (southern Koryak Upland, western Kamchatka) suggests that the Okhotsk-Chukot volcanogenic belt and fragments of the Uda
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d68216d27a2993a659cc6650f03cc6a9
https://doi.org/10.1023/a:1010458120285
https://doi.org/10.1023/a:1010458120285
Publikováno v:
Tectonics. 19:834-851
The remnants of ancient island arcs are exposed in the Achayvayam-Valagina and East Peninsulas tectonic zones of the Olutor-Kamchatka region, northeast Russia. Geochemically, Late Cretaceous to Paleogene island arc complexes of the East Peninsulas zo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a510b7a6e2d7bea93a37aadf3419e54
https://doi.org/10.1029/1998tc001087
https://doi.org/10.1029/1998tc001087
Late Cretaceous paleomagnetic data from the Median Range of Kamchatka, Russia: tectonic implications
Publikováno v:
Earth and Planetary Science Letters. 163:235-246
A Late Cretaceous island arc complex was sampled for paleomagnetic study in the northern part of the Median Range of Kamchatka. In most samples, thermal demagnetization in 12–18 steps revealed either a reversed characteristic remanent magnetization
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7cd74ffb096d7817086d94d7d4d41320
https://doi.org/10.1016/s0012-821x(98)00190-3
https://doi.org/10.1016/s0012-821x(98)00190-3