Seismicity of the Bering Strait region: Evidence for a Bering block

Mackey, K. G.; Fujita, Kazuya; Gunbina, L. V.; Kovalev, Valentin N.; Imaev, V. S.; Козьмин, Б. М.; Имаева, Л. П.

doi:10.1130/0091-7613(1997)025<0979:sotbsr>2.3.co;2

Cited by 99 publications

(97 citation statements)

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“…Mackey et al (1997) have recently de"ned the Bering Sea, Chukotka Peninsula, Seward Peninsula and part of western Alaska as an independent tectonic block that has been rotated clockwise in tandem with the northwest subduction of the Paci"c plate. Rotation of the Bering Block is thought to have been initiated 5.5 My ago providing a realistic mechanism for the initial extension, faulting and submergence of the Bering Strait region.…”

Section: First Submergence Of Bering Straitmentioning

confidence: 99%

New perspectives on Beringian Quaternary paleogeography, stratigraphy, and glacial history

Brigham‐Grette

2001

Quaternary Science Reviews

115

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Aspects of the paleogeography, stratigraphy, and glacial history of Beringia have been greatly revised over the past 15}20 yr. Access to North East Russia, in particular, has provided the opportunity to evaluate the Beringia landscape as a contiguous subcontinent during the Quaternary. For the "rst time, new research has made clearer the connection between tectonic forces and the submergence of the Bering Strait during the middle Pliocene. Revisions in the regional stratigraphy of glacial and interglacial deposits in northwest Alaska and northeast Russia provide a new foundation for assessing the causes for di!erences in glacial ice extent through time. The consensus of all "eld workers veri"es that glacial ice throughout most of Beringia was of very limited extent during the last glacial maximum. The onset of regional glaciation during the waning stages of the last interglaciation is clearly out of phase with glaciation at lower latitudes. Despite the lack of much glacial activity during the early Holocene, Alaska contains a rich record of late Holocene glacial response to Neoglacial cooling. Changes in the Holocene environment of Beringia likely had a profound a!ect on early inhabitants. The curiosity-driven vision and spirit of both David Hopkins and the late Troy Pewe have had a profound in#uence on Arctic paleoenvironmental research.

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Section: First Submergence Of Bering Straitmentioning

confidence: 99%

New perspectives on Beringian Quaternary paleogeography, stratigraphy, and glacial history

Brigham‐Grette

2001

Quaternary Science Reviews

115

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“…В пределах сегмента развита система круп-ных взбросов-сдвигов северо-восточного прости-рания, современная активность которых определя-ется крупными сейсмическими событиями 1988, 1991 и 2006 гг. Их фокальные механизмы также подтверждают взбросовую природу этих землетря-сений [Lander et al, 1996[Lander et al, , 2007Mackey et al, 1997].…”

Section: рис 5 схема сейсмотектоники зоны черскогоunclassified

“…Современная тектоническая позиция, проявления сейсмичности и кинематический тип сейсмотектонических деформаций региона связа-ны с образованием в позднем мезозое рифта Бе-рингова моря [Nakamura et al, 1980;Mackey et al, 1997;Nokleberg еt al., 2000;Parfenov et al, 2001]. Рифт представляет собой зону растяжения, кото-рая возникла между окончаниями двух крупных систем взбросов и правых сдвигов на Корякском нагорье -Чукотке и правых сдвигов Западной Аляски (см.…”

Section: Fig 6 Seismotectonics Of the Koryak Segment (Modified Afterunclassified

Geodynamic Activity of Modern Structures and Tectonic Stress Fields in Northeast Asia

Имаева¹,

Гусев²,

Imaev³

et al. 2017

Geodin. tektonofiz.

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Abstract:Based on the analysis of changes in the stress-strain state of the crust at the boundary of the Eurasian and North American tectonic plates, we develop a dynamic model of the main seismogenerating structures in Northeast Asia. We have established a regularity in changes of geodynamic regimes within the interplate boundary between the Kolyma-Chukotka crustal plate and the Eurasian, North American and Pacific tectonic plates: spreading in the Gakkel Ridge area; rifting in the Laptev Sea shelf; a mixture of tectonic stress types in the Kharaulakh segment; transpression in the Chersky seismotectonic zone, in the segment from the Komandor to the Aleutian Islands, and in the Koryak segment; and crustal stretching in the Chukotka segment.

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“…There were some papers that inspired to search scientific explanations about the Cuban seismicity as (Makarov and Schukin, 1976;) Sibson, 1985;Spiridonov and Grigorova, 1980). The results of (Assinovskaya and Soloviev, 1994;Backmanov and Rasskazov, 2000;Guelfand et al, 1976;Gvshiani et al, 1987;Mackey et al, 1977;Sherman and San`kov, 2010;Stein and Yeats, 1989;Zhidkov, 1985;Zhidkov et al, 1975) contributed to develop the methodology of the active structures. In order to obtain the comprehension of the earthquakes localization on intraplate zones were used (Campbell, 1978;Jonston, 1989;Johnston and Kanter, 1990;Leonov, 1995;LeRoy and Mauffret, 1996;Liu and Zoback, 1977;Sbar and Sykes, 1973;Stein, 1999;Sykes, 1978;Zoback, 1992).…”

Section: The Geodynamic Modelmentioning

confidence: 99%