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Clockwise rotation of SW Japan and timing of Izanagi–Pacific ridge subduction revealed by arc migration
Igneous rocks associated with the Cretaceous to Paleogene volcanic arc in SW Japan show ages that young from west to east in a direction parallel to...
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Lower cretaceous missing volcanic arc. A migrating arc, central Patagonian cordillera, Chile: Detrital zircon U–Pb geochronology
New U–Pb detrital zircon ages from seven samples from the Lower Cretaceous Katterfeld and Apeleg formations and Divisadero Group of Central Patagonia...
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Low-magnitude seismic swarms in the Calabrian Arc (Italy)
Seismic swarms of low magnitude earthquakes occur frequently in the Calabrian Arc. During the last few years, several earthquakes of magnitude up to M
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Magmatic evolution of the migrating central Urumieh–Dokhtar arc, Iran: implications for magma production
The Cenozoic Avaj volcano-plutonic rocks in central Urumieh-Dokhtar magmatic arc (UDMA) encompass gabbro, and basalt to rhyolite, chemically akin to...
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Ascent-driven differentiation: a mechanism to keep arc magmas metaluminous?
Arc magmatism is fundamental to the generation of new continental or island arc crust. However, the mechanisms that add to the chemical complexity of...
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Tectonic controls on the origin and segmentation of the Cascade Arc, USA
The magmatic response above subducting ocean lithosphere can range from weak to vigorous and from a narrow zone to widely distributed. The small and...
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A possible mechanism for spontaneous cyclic back-arc spreading
Back-arc spreading is a non-steady-state process exemplified by the repeated cycles of spreading of the South Fiji and the Lau Basins behind the...
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Sparsity-promoting wide-angle least-squares one-way migration
For structural geology and geophysical exploration, it is of particular importance to get accurate images of salt domes, especially the subsalt...
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PP- and PS-wave migration of OBN seismic data from rugged seabeds
Multicomponent seismic exploration offers advantages in precisely describing complicated geological structures compared with conventional PP-wave...
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Coseismic and Tectonic Time-Scale Deformations of an Island Arc Based on the Studies of the East Coast of the Kamchatka Peninsula (Far East, Russia)
AbstractThe geologic structure of the late Holocene accumulative marine terrace on the Kamchatka Bay coast (Kamchatka Peninsula) has been studied....
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H2O-induced sedimentary carbon migration from subducting slabs to the forearc mantle
Carbon in sedimentary carbonates dominates the global carbon input flux in subduction zones, the fate of which makes an impact on the global carbon...
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Migration imaging processing of subgrade cavity GPR detection based on TUFK method
Timely and accurate detection and identification of cavities under urban roads is the key to road safety. Due to the inability to obtain accurate...
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Insights into the seismogenic structures of the arc-continent convergent plate boundary in eastern Taiwan
The doubly vergent orogen in Taiwan is a relatively young and active arc-continent collision caused by the convergence of Eurasian and Philippine Sea...
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Neotectonics at the SE Continental Margin of the Korean Peninsula: Implications for the Back-Arc Region Behind the SW Japan Arc
The geological evolution of the SE continental margin of the Korean Peninsula resulted from crustal extension with back-arc rifting to spreading...
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Gas migration signatures over the volcanic cratered seamount, off the Nicobar Islands in the Andaman Sea
The submarine volcanic arc off-Nicobar is seismologically very active with numerous earthquake swarms reported after the tsunamigenic 26th December...
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Modelling of insitu channel migration vis-à-vis bank stability of Brahmani River, Odisha
The process of insitu migration of river channels involves the alteration of morphological parameters, which affects river morphodynamics at both...
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Subsurface structure of Bali Island inferred from magnetic and gravity modeling: new insights into volcanic activity and migration of volcanic centers
Bali island is part of the Sunda volcanic arc with an active volcano at its center. The Buyan-Bratan caldera, the Batur volcano, and the Agung...
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Platinum-group element geochemistry of the shoshonitic igneous suite of Vulcano (Aeolian Arc, Italy): implications for chalcophile element fertility of arc magmas
Platinum-group element (PGE) geochemistry of arc-related magmas can be used to constrain the timing of sulfide saturation, which plays a critical...
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Petrological and chemical evidence for polybaric differentiation across the preserved middle crustal plutonic column of the Famatinian arc, Argentina
This study investigates the formation of the middle layer of the Earth's crust in the Early Ordovician Famatinian arc. We focus on the Valle...
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Arc–Back Arc Cohabitation and Associated Bimodal Volcanism: Evidence from Neoarchean Raichur Greenstone Belt, Eastern Dharwar Craton, India
The Raichur greenstone belt of eastern Dharwar craton preserves the mafic and felsic volcanic rocks that are characterized as bimodal suite in which...