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Izanagi Plate

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Journal Article
Journal: Geology
Published: 28 April 2021
Geology (2021) 49 (8): 952–957.
...Toru Yamasaki; Gen Shimoda; Kenichiro Tani; Jinichiro Maeda; Futoshi Nanayama Abstract Recent reconstructions of global plate motions suggest that the Izanagi-Pacific Ridge was subducted along the eastern margin of Eurasia at ca. 50 Ma. In the Hidaka magmatic zone (HMZ), which was located...
FIGURES | View All (4)
Journal Article
Journal: GSA Bulletin
Published: 27 February 2024
GSA Bulletin (2024) 136 (9-10): 3850–3860.
... on the configurative, compositional, and isotopic evidences, the magmatic belts record the fingerprints of the slab window generated by disassembly of the paleo-ridge between the Paleo-Pacific and Izanagi plates at ca. 150–135 Ma. During this time, the Paleo-Pacific plate rolled back beneath the eastern margin...
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Series: GSA Special Papers
Published: 01 January 1985
DOI: 10.1130/SPE206-p1
... A model is presented for the displacement history between western North America, eastern Eurasia, and adjacent oceanic plates (Pacific, Farallon, Izanagi, Kula, and Phoenix) for the past 180 million years. The model is based on the assumption that the hotspots in the Atlantic region have...
Journal Article
Journal: GSA Bulletin
Published: 05 May 2023
GSA Bulletin (2024) 136 (1-2): 171–183.
... America are related to transpression caused by high-rate oblique subduction with intermediate–high dip angles of the Izanagi and Farallon plates, respectively. In contrast, the ~105-m.y.-old porphyry-epithermal belt in Southeast China was produced by oblique subduction of the Izanagi Plate with low...
FIGURES | View All (9)
Image
Schematic geodynamic evolution of the eastern North China Craton (NCC). (A)...
Published: 04 February 2020
Figure 13. Schematic geodynamic evolution of the eastern North China Craton (NCC). (A) During the Late Jurassic, D 1 thrusting formed in response to rapid, low-angle, oblique subduction of the Izanagi Plate. (B) During the earliest Early Cretaceous, D 2 sinistral faulting occurred in response
Image
Figure 1. <span class="search-highlight">Plate</span> reconstruction explaining how part of the Hawaiian hotspot ...
Published: 01 May 2007
Figure 1. Plate reconstruction explaining how part of the Hawaiian hotspot track could have become preserved in the Bering Sea. Arrows indicate plate velocities. Computed hotspot tracks are shown on Pacific plate for ages younger than 78 Ma, and on Izanagi-Kula–North American plate for ages older
Journal Article
Journal: GSA Bulletin
Published: 22 February 2024
GSA Bulletin (2024) 136 (9-10): 3705–3734.
...Jinlong Ni; Ruijie Wang; Junlai Liu; Zhengzheng Wang; Chaoyang Li; Lei Ji; Jian Zhang Abstract The late Mesozoic subduction of the paleo-Pacific plate (Izanagi plate) beneath Eurasia involved complex changes in the direction and angle of subduction, which have been controversial in recent decades...
FIGURES | View All (17)
Published: 01 January 2007
DOI: 10.1130/2007.2430(23)
.... Plate reorganizations in the Late Cretaceous resulted from the breakup of the Phoenix and Izanagi plates through collision of the Pacific-Phoenix ocean ridge with the southwest margin of the basin and development of island arc–marginal basin systems in the northwestern part of the basin. The Pacific...
Journal Article
Journal: Geology
Published: 01 May 2007
Geology (2007) 35 (5): 407–410.
...Figure 1. Plate reconstruction explaining how part of the Hawaiian hotspot track could have become preserved in the Bering Sea. Arrows indicate plate velocities. Computed hotspot tracks are shown on Pacific plate for ages younger than 78 Ma, and on Izanagi-Kula–North American plate for ages older...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 March 2009
Economic Geology (2009) 104 (2): 303–321.
..., is not supported by the development of extensional basins in the region. From the Late Jurassic to Cretaceous, eastern China was closely associated with subduction of the Pacific plate in the south and the Izanagi plate in the north. The midocean ridge (MOR) between these two plates was drifting toward and likely...
FIGURES | View All (5)
... paleoreconstructions were developed based on the newly received and published data, in accordance with which the Kiselevka block: (1) in the range of 135–105 Ma was moving on the Izanagi plate northwestward at a rate of 15–20 cm/yr up to the eastern edge of Eurasia, thus covering over 5000 km; and (2) in the range...
Journal Article
Published: 01 May 2010
The Journal of Geology (2010) 118 (3): 277–293.
... a transpressive regime along the ECCM during the Late Jurassic. It is inferred that the switch from Late Jurassic transpression to Early Cretaceous extension is due to a shift from oblique, shallow subduction of the Izanagi Plate to orthogonal, steep subduction of the Pacific Plate. Normal faulting...
FIGURES | View All (8)
Image
(A) Map of the principal Yanshanian thrust, strike-slip, and fold structure...
Published: 18 September 2019
Figure 11. (A) Map of the principal Yanshanian thrust, strike-slip, and fold structures in North China and exposures of Early–Middle Jurassic arc batholithic rocks in the Korean Peninsula (e.g., Kim et al., 2015 ). The position of the Izanagi and eastern Asian plate boundary is based
Journal Article
Journal: Economic Geology
Published: 01 March 2023
Economic Geology (2023) 118 (2): 509–518.
... to an extensional setting following Triassic intracontinental orogeny and to Late Jurassic-Early Cretaceous extension associated with Izanagi plate rollback, respectively. † Corresponding author: e-mail, [email protected] 22 10 2021 21 05 2022 © 2023 Society of Economic Geologists...
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Journal Article
Journal: Economic Geology
Published: 01 May 2020
Economic Geology (2020) 115 (3): 671–685.
...Jun Deng; Kun-Feng Qiu; Qing-Fei Wang; Richard Goldfarb; Li-Qiang Yang; Jian-Wei Zi; Jian-Zhen Geng; Yao Ma Abstract The Jiaodong gold province, the largest gold producer in China, formed in a setting dominated by a 30-m.y. episode of Izanagi plate rollback and widespread extension, concomitant...
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Journal Article
Published: 01 August 2005
Bulletin of the Seismological Society of America (2005) 95 (4): 1516–1534.
... discrepancy is found in the Gyeongsang basin formed in a retroarc setting by the subduction of the Izanagi Plate in the early Cretaceous. A thick crust observed in the basin may be caused by two factors—maturity of the basin and underplating of magma materials. Average crustal velocities vary from 6.02 km/sec...
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Series: Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.227.01.14
EISBN: 9781862394759
... to flattening across the metamorphic belt. We hypothesize that the data are most reasonably explained by a model of counter-flow in the subduction channel. The counter-flow was induced by a left-lateral oblique subduction of the oceanic (Izanagi) plate, which was strongly coupled with the subducting sediments...
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Image
Tectonic evolution of Sikhote-Alin (Russian Far East) to Japan during the I...
Published: 20 August 2019
Figure 4. Tectonic evolution of Sikhote-Alin (Russian Far East) to Japan during the Izanagi-Pacific ridge-trench intersection in the early Cenozoic based on this study. PAC—Pacific plate; IZA—Izanagi plate. (A) Mid-Cretaceous to Paleocene arc magmatism was characterized by more-enriched isotopic
Image
Models for the evolution of the East China continental margin.  a , Extensi...
Published: 01 May 2010
in the Late Jurassic due to oblique, shallow subduction of the Izanagi Plate. F = fault.
Image
Figure 2. Computed Hawaiian hotspot tracks in the Bering Sea for different ...
Published: 01 May 2007
with change from Izanagi to Kula plate motion and transfer from Kula to North American plate as indicated, and Pacific and African plate motions in the moving hotspot reference frame. Red line with diamonds is computed with African plate motion in the fixed (instead of moving) hotspot reference frame after 47