Growth of forearc highs and basins in the oblique Sumatra subduction system
Based on structural deformation analysis in the oblique Sumatra subduction system, we review uplift mechanisms of the forearc high and formation of the forearc basin.
Maruf M Mukti, Haryadi Permana
exaly +4 more sources
Understanding subduction infancy to mature subduction in Southwest Japan via the self-consistent formation of a weak slab interface [PDF]
The weak slab interface controls long-term subduction dynamics. A weak hydrous layer at the slab interface promotes mechanical decoupling between the forearc mantle and the subducting slab and converts a hot forearc mantle to a cold mantle.
Changyeol Lee, YoungHee Kim
doaj +2 more sources
Unraveling the diversity of Arc volcanism and deep low-frequency tremors in Southwest Japan from numerical modeling [PDF]
Differences in slab dehydration and fluid transport influence the distribution of magmatism and deep low-frequency tremors in subduction zones. Southwest Japan, particularly Kyushu and Shikoku/Chugoku, exhibits significant along-arc variation in the ...
Goeun Ha, Changyeol Lee, YoungHee Kim
doaj +2 more sources
Reestimation of slab dehydration fronts in Kuril-Kamchatka using updated global subduction zone thermal structures [PDF]
Summary: Previous subduction thermal models are inconsistent with the values of forearc heat flow (50–140 mW/m2) and global P‒T conditions of exhumed rocks, both suggesting a shallow environment 200–300°C warmer than model predictions. Here, we revaluate
Weiling Zhu +6 more
doaj +2 more sources
Normal Faulting Along the Kythira-Antikythira Strait, Southwest Hellenic Forearc, Greece
Upper-plate normal faults along forearcs often accumulate slip during >Mw 6 earthquakes. Such normal faults traverse the forearc of the Hellenic Subduction System (HSS) in Greece and are the focus of this study. Here, we use detailed field-mapping and
Violeta Veliz-Borel +4 more
doaj +1 more source
High‐Pressure Na‐Ca Carbonates in the Deep Carbon Cycle
This book is Open Access. A digital copy can be downloaded for free from Wiley Online Library.
Explores the behavior of carbon in minerals, melts, and fluids under extreme conditions
Carbon trapped in diamonds and carbonate-bearing rocks in subduction zones are examples of the continuing exchange of substantial carbon ...
Sergey Rashchenko +2 more
wiley +2 more sources
Phanerozoic Large Igneous Province, Petroleum System, and Source Rock Links
Exploring the links between Large Igneous Provinces and dramatic environmental impact
An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Steven C. Bergman +2 more
wiley +1 more source
The southern Cascadia forearc undergoes a three-stage tectonic evolution, each stage involving different combinations of tectonic drivers, that produce differences in the upper-plate deformation style.
Kirsty A. McKenzie +2 more
doaj +1 more source
The fate of fluids released from subducting slab in northern Cascadia [PDF]
Large amounts of water carried down in subduction zones are driven upward into the overlying forearc upper mantle and crust as increasing temperatures and pressure dehydrate the subducting crust.
K. Ramachandran, R. D. Hyndman
doaj +1 more source
Seismic Anisotropy Analysis Beneath Sumatra Revealed by Shear-Wave Splitting
DOI: 10.17014/ijog.4.3.169-179A shear-wave splitting analysis was determined to observe anisotropic structures of an upper mantle layer beneath Sumatra.
Arya Dwi Candra +2 more
doaj +1 more source

