Ocean-continent transition architecture and breakup mechanism at the mid-northern South China Sea
C Zhang, Z Sun, G Manatschal, X Pang, S Li… - Earth-Science …, 2021 - Elsevier
Abstract Ocean-Continent Transition (OCT) located between the edge of the continental and
unequivocal oceanic crusts is an ideal laboratory to understand one of the most fundamental …
unequivocal oceanic crusts is an ideal laboratory to understand one of the most fundamental …
The Cretaceous volcanism of the Songliao Basin: Mantle sources, magma evolution processes and implications for the NE China geodynamics-A review
Continental rifts result from the simultaneous action of shallow processes such as the
thinning of the lithosphere, and deeper processes related to the dynamics of the mantle. The …
thinning of the lithosphere, and deeper processes related to the dynamics of the mantle. The …
[图书][B] Volcano-tectonic processes
V Acocella - 2021 - Springer
Among the various university courses I took for my geoscience degree, volcanology and
structural geology motivated me by far the most. Volcanoes and deformed rocks are indeed …
structural geology motivated me by far the most. Volcanoes and deformed rocks are indeed …
Microseismicity and lithosphere thickness at a nearly-amagmatic oceanic detachment fault system
Oceanic detachment faults play a central role in accommodating the plate divergence at
slow-ultraslow spreading mid-ocean ridges. Successive flip-flop detachment faults in a …
slow-ultraslow spreading mid-ocean ridges. Successive flip-flop detachment faults in a …
Controls on the magmatic fraction of extension at mid-ocean ridges
JA Olive, P Dublanchet - Earth and Planetary Science Letters, 2020 - Elsevier
The fraction M of plate separation accommodated by magma emplacement at mid-ocean
ridges has been recognized as the main control on seafloor spreading modes, yet the …
ridges has been recognized as the main control on seafloor spreading modes, yet the …
Mantle serpentinization and associated hydrogen flux at North Atlantic magma-poor rifted margins
Z Liu, M Perez-Gussinye, J García-Pintado… - …, 2023 - pubs.geoscienceworld.org
Mantle serpentinization influences the rheology of altered peridotites and the global fluxes of
energy and volatiles, the generation of seafloor and sub-seafloor chemolithotrophic life, and …
energy and volatiles, the generation of seafloor and sub-seafloor chemolithotrophic life, and …
Oxidizing fluids associated with detachment hosted hydrothermal systems: Example from the Suye hydrothermal field on the ultraslow-spreading Southwest Indian …
S Liao, C Tao, JW Jamieson, J Liu, C Zhu… - … et Cosmochimica Acta, 2022 - Elsevier
The redox state of hydrothermal fluids on mid-ocean ridges, which is indirectly affected by
the depth of hydrothermal circulation and crustal permeability, plays an important role on the …
the depth of hydrothermal circulation and crustal permeability, plays an important role on the …
Beyond spreading rate: Controls on the thermal regime of mid-ocean ridges
The thermal state of mid-ocean ridges exerts a crucial modulation on seafloor spreading
processes that shape~ 2/3 of our planet's surface. Standard thermal models treat the ridge …
processes that shape~ 2/3 of our planet's surface. Standard thermal models treat the ridge …
[HTML][HTML] Evolution of enhanced magmatism at the ultraslow spreading Southwest Indian Ridge between 46 E and 53.5 E
Abstract The Indomed-Gallieni supersegment (46-52° E) of the Southwest Indian Ridge
(SWIR) has been of interest as a melt-rich endmember of ultraslow spreading mid-ocean …
(SWIR) has been of interest as a melt-rich endmember of ultraslow spreading mid-ocean …
780 thousand years of upper‐crustal construction at a melt‐rich segment of the ultraslow spreading Southwest Indian Ridge 50° 28′ E
Melt supply at the ultraslow‐spreading Southwest Indian Ridge (SWIR) has been shown to
vary from nearly amagmatic, leading to ultramafic seafloor, to magmatically robust …
vary from nearly amagmatic, leading to ultramafic seafloor, to magmatically robust …