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Thus, we rule out the involvement in rodingitization of seawater modified in a hydrothermal system driven by mafic magmatism in or near an oceanic zone of extension.
West of 102°W, the boundary swings away from the continental margin and becomes a diffuse zone of extension and magmatic activity encompassing the Marie Byrd Seamounts.
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Inferred temperature conditions for ductile mélange (extension veins only in sandstone); the ductile brittle transition zone (coexistence of extension veins in sandstone blocks and shear vein) and brittle deformation (shear vein) are also indicated.
The Euphrates Graben is a fault-bounded failed rift that has been studied extensively by Litak et al. 1997 showed that the Euphrates Fault System is a related, but less-deformed zone of an extension that extends from the Iraqi border in the southeast to the Turkish border in the northwest and includes the Euphrates Graben.
Two integrated high temperature ultrasonic transducers (HTUTs) were fabricated on both sides of diagnosing zone of T-shape extension nozzle for process monitoring at elevated temperature real-time, non-intrusively and non-destructively.
These findings imply that foreshocks and partially also mainshock are driven by stresses of the NE SW shear zone (western extension of the MTL), while aftershocks are mostly related to the N S extensional stress regime of Beppu Shimabara graben (Kamata and Kodama 1994), being triggered by the mainshock.
Kyushu Island is characterized by active volcanoes (Aso, Unzen, Kirishima, and Sakurajima) and a shear zone (western extension of the median tectonic line).
Along the graben, a shear zone (western extension of the median tectonic line) is present under the north south extensional stress regime where both normal faulting and strike-slip earthquakes have occurred (Matsumoto et al. 2015).
Each zone consists of a pair of extension fractures or a pair of normal faults, with lengths from metres to kilometres.
In the actively extending Red Sea margin of eastern Eritrea, which lies at the Red Sea/Danakil Gulf of Aden and the East African rift triple junction zone, the geometry and kinematics of extension are complex and poorly defined due to large data gaps.
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