Late Mesozoic and Cenozoic volcanism of the East Sikhote-Alin area (Russian Far East): A new synthesis of geological and petrological data

Martynov, Yurii A.; Ханчук, А. И.; Grebennikov, A. V.; Chashchin, A. A.; Попов, В. К.

doi:10.1016/j.gr.2017.01.005

Cited by 37 publications

(15 citation statements)

References 67 publications

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“…The N-S-trending subduction-related terranes that form the basement of central Hokkaido continue northward on the island of Sakhalin. The Cretaceous-Paleocene East Sikhote-Alin arc forms the volcanic arc associated with the subduction below Hokkaido and Sakhalin (Kemkin et al, 2016;Martynov et al, 2017;Nokleberg et al, 2000;Parfenov et al, 2009;Tang et al, 2016;Figures 2 and 4). Structurally above the units interpreted to belong to Eurasia, or on Hokkaido separated from Eurasia by a strike-slip fault, are the Late Cretaceous to early Paleogene East Sakhalin-Nemuro island-arc units found on east Hokkaido and east Sakhalin (e.g., Nokleberg et al, 1996Nokleberg et al, , 2000Ueda, 2016;Zharov, 2005; Figures 2-4).…”

Section: 1029/2018tc005164mentioning

confidence: 99%

Reconstruction of Subduction and Back‐Arc Spreading in the NW Pacific and Aleutian Basin: Clues to Causes of Cretaceous and Eocene Plate Reorganizations

2019

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The Eocene (~50–45 Ma) major absolute plate motion change of the Pacific plate forming the Hawaii‐Emperor bend is thought to result from inception of Pacific plate subduction along one of its modern western trenches. Subduction is suggested to have started either spontaneously, or result from subduction of the Izanagi‐Pacific mid‐ocean ridge, or from subduction polarity reversal after collision of the Olyutorsky arc that was built on the Pacific plate with NE Asia. Here we provide a detailed plate‐kinematic reconstruction of back‐arc basins and accreted terranes in the northwest Pacific region, from Japan to the Bering Sea, since the Late Cretaceous. We present a new tectonic reconstruction of the intraoceanic Olyutorsky and Kronotsky arcs, which formed above two adjacent, oppositely dipping subduction zones at ~85 Ma within the north Pacific region, during another Pacific‐wide plate reorganization. We use our reconstruction to explain the formation of the submarine Shirshov and Bowers Ridges and show that if marine magnetic anomalies reported from the Aleutian Basin represent magnetic polarity reversals, its crust most likely formed in an ~85‐ to 60‐Ma back‐arc basin behind the Olyutorsky arc. The Olyutorsky arc was then separated from the Pacific plate by a spreading ridge, so that the ~55‐ to 50‐Ma subduction polarity reversal that followed upon Olyutorsky‐NE Asia collision initiated subduction of a plate that was not the Pacific. Hence, this polarity reversal may not be a straightforward driver of the Eocene Pacific plate motion change, whose causes remain enigmatic.

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Section: 1029/2018tc005164mentioning

confidence: 99%

Reconstruction of Subduction and Back‐Arc Spreading in the NW Pacific and Aleutian Basin: Clues to Causes of Cretaceous and Eocene Plate Reorganizations

2019

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“…Recycling of the oceanic lithosphere substance in subduction zones (after [Winter, 2001;Richards, 2011]). Yarmolyuk et al, 2013;Perepelov, 2008Perepelov, , 2014Flerov et al, 2016;Martynov et al, 2017].…”

Section: Figmentioning

confidence: 99%

“…Это показано на примере Курило-Камчатской островодужной системы [Khanchuk, Martynov, 2011;Martynov et al, 2017;Perepelov, 2008Perepelov, , 2014. Было Рис.…”

Section: субдукционный и плюмовый магматизм в островодужных системахunclassified

“…Известным эталонным объектом магматизма зон скольжения литосферных плит является калифорнийская окраина Северной Америки [Zonenshain et al, 1976], а также изученная в последнее время территория Восточно-Сихотэ-Алинского вулканического пояса [Khanchuk, Martynov, 2011;Martynov, Khanchuk, 2013;Martynov et al, 2017]. Было установлено, что в кайнозое определяющую роль в формировании западно-тихоокеанской окраины, в том числе и территории Восточного Сихотэ-Алиня, играли не только субдукционные процессы, но и тектоническая перестройка всей Северо-Восточной Азии в результате взаимодействия Индостанской, Азиатской и Тихоокеанской плит с участием мантийных плюмов.…”

Section: субдукционный и плюмовый магматизм в островодужных системахunclassified

“…История геодинамического развития Восточно-Сихотэ-Алинского и Японского регионов показана на рисунке 11 [Martynov, Khanchuk, 2013;Martynov et al, 2017]: (а) -на данной территории в зоне столкновения Индостанской и Тихоокеанской плит в начале юры возникла островодужная система, которая развивалась до конца мела (95-65 млн лет); (б) -в последующем (55-15 млн лет) в результате конвекции в астеносфере и деплетированной верхней мантии возникла трансформная зона растяжения. Слэб был разорван и сдвинут, и в это «окно» проник горячий астеносферный материал, который привел к одновременному островодужному и плюмовому магматизму, а на границе континенттрансформная зона возник турбидитовый бассейн; (в) -в конце миоцена -плиоцене (12-4 млн лет) во фронтальной части трансформной границы возникла новая вулканическая дуга и образовался задуговый бассейн.…”

Section: субдукционный и плюмовый магматизм в островодужных системахunclassified

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Relationship Between Subduction‐related and Plume Magmatism at the Active Boundaries of Lithospheric Plates in the Interaction Zone of the Siberian Continent and Paleoasian Ocean in the Neoproterozoic and Paleozoic

Гордиенко

2019

Geodin. tektonofiz.

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This paper is focused on the relationship between plate-and plume-tectonic processes during the formation of Neoproterozoic and Vendian-Paleozoic island-arc systems and active continental margins in the interaction zone of the Siberian continent and Paleoasian Ocean (PAO). In this study, we use our own materials collected in the long-term research of the Central Asian Orogenic Belt (CAOB) and the published models showing convection in the asthenosphere and mantle, subduction-related and plume magmatism at the Cenozoic active margins of the Western Pacific and California types. It is clearly shown that subduction-related magmatism of the Paleoasian Ocean active margins should not be considered separately from plume magmatism. These interrelated processes played a major role in the CAOB formation. Based on the reconstructed Neoproterozoic, Vendian-Early and Middle Paleozoic paleogeodynamic features, 25 island-arc systems of PAO are characterized. These island arcs are related to the occurrence of more than 30 plume magmatism areas. At the active margin of the Siberian continent, there are numerous fields of intraplate magmatism in riftogeneous structures. Such fields of various scales not related to subduction zones, especially at the final Late Paleozoic stage. All the major stages of the CAOB development, including the Cambrian-Ordovician collision stage, are clearly correlated with plume magmatism. Considering a revealed combination of the island arcs and the plume magmatism areas, there are grounds to suggest that the development of the entire Neoproterozoic-Paleozoic region of Central Asia was related to the activity of mantle plumes.

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Evolution of the Paleo–Asian Ocean in south‐eastern Inner Mongolia, China: Evidence from zircon U–Pb ages, Hf isotopes data and specific deformation of the Linxi and Sunjiafen formations

Huang

Liu

et al. 2023

Geological Journal

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The crystallization age of the Sunjiafen Formation volcanic rocks is 253.9 ± 1.1 Ma. Geochemical data show that these volcanic rocks belong to the shoshonitic and metaluminous series and have high Sr and low Y contents (461–582 and 5.60–6.74 ppm, respectively), MgO = 1.32–2.65 wt%, and Na2O/K2O = 0.81–1.40. In MgO−SiO2, Cr−SiO2, Sr/Y−Y and (La/Yb)N−YbN diagrams, data for the samples plot in the adakite and “adakite related to thickened lower crust” fields. As such, we suggest that the Sunjiafen Formation C−type adakitic andesites formed in a compressional tectonic setting. The youngest age (youngest peak age) of two sandstone samples from the Linxi Formation are 251 Ma (257 Ma) and 237 Ma (254 Ma). Detrital zircons with ages of >1500 Ma have εHf(t) values of −5.87 to +6.31. A comparison of the age spectra and εHf(t) values of the detrital zircons in the Linxi Formation with those of igneous zircons from the Central Asian Orogenic Belt and North China Craton indicates the formation was derived from both the belt and the craton. We identified “Jura–type Folds” that formed in peripheral foreland basin in the Linxi Formation, and along with plant fossil fragments (Paracalamites frigidus). These and previously published results indicate the Paleo–Asian Ocean closed along the Xar Moron–Changchun Suture zone during the Late Permian. The study area was in a continuous compressional setting during the Late Permian and formed a peripheral foreland basin that was related to continent–continent collision.

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Late Mesozoic and Cenozoic volcanism of the East Sikhote-Alin area (Russian Far East): A new synthesis of geological and petrological data

Cited by 37 publications

References 67 publications

Reconstruction of Subduction and Back‐Arc Spreading in the NW Pacific and Aleutian Basin: Clues to Causes of Cretaceous and Eocene Plate Reorganizations

Reconstruction of Subduction and Back‐Arc Spreading in the NW Pacific and Aleutian Basin: Clues to Causes of Cretaceous and Eocene Plate Reorganizations

Relationship Between Subduction‐related and Plume Magmatism at the Active Boundaries of Lithospheric Plates in the Interaction Zone of the Siberian Continent and Paleoasian Ocean in the Neoproterozoic and Paleozoic

Evolution of the Paleo–Asian Ocean in south‐eastern Inner Mongolia, China: Evidence from zircon U–Pb ages, Hf isotopes data and specific deformation of the Linxi and Sunjiafen formations

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