Natural hydrogen in the volcanic-bearing sedimentary basin: Origin, conversion, and production rates. [PDF]
Liu Q+11 more
europepmc +1 more source
Mantle Exhumation and Post‐Rift Magmatism at an Oblique Magma‐Poor Continental Margin
Abstract Continental breakup is a fundamental tectonic process, which leads to seafloor spreading and the generation of oceanic crust. However, the current understanding of continental margins, based largely on 2‐D seismic transects, is inadequate to capture the spatial complexity of crustal evolution.
Jie Chen+3 more
wiley +1 more source
Northern Scandinavian mountains supported by a low-grade eclogitic crustal keel. [PDF]
Kahraman M+5 more
europepmc +1 more source
Mercury's Tidal Love Number h2 ${h}_{2}$ From Co‐Registration of MLA Profiles
Abstract Due to its eccentric orbit, Mercury experiences a varying gravitational pull from the Sun along its orbit, leading to periodic surface tidal deformation. The previous measurement of Mercury's tidal h2 ${h}_{2}$ by Bertone et al. (2021, https://doi.org/10.1029/2020je006683) is based on minimizing height differences at cross‐overs of the Mercury
Haifeng Xiao+5 more
wiley +1 more source
Publisher Correction: Diversities of chromite mineralization induced by chemo-thermal evolution of the mantle during subduction initiation. [PDF]
Zhang PF+6 more
europepmc +1 more source
Abstract Pressure and temperature increase with depth, modifying the microstructure of crustal rocks. The opening or closing of micro‐ and macrocracks resulting from variations in the in‐situ conditions influences the permeability of crustal rocks. While confining pressure is known to close pre‐existing cracks, reducing permeability, the influence of ...
L. Carbillet+3 more
wiley +1 more source
Periodic instability and restoration of cratonic lithosphere. [PDF]
Liu L+5 more
europepmc +1 more source
Abstract At the subduction zone interface, a combination of mechanical deformation and (fluid‐mediated) chemical mixing of oceanic crust, sediment and mantle lithologies yields heterogeneous mélange lithologies. These mélanges have compositions and metamorphic mineral assemblages dissimilar to their endmember source lithologies, resulting in a ...
Benjamin Z. Klein, Mark D. Behn
wiley +1 more source
Sources and processes in arc magmatism: the crucial role of water [PDF]
Elburg, Marlina
core +1 more source
Magnetotelluric evidence for the deep causes of different eruptive styles of Changbaishan Tianchi and Longgang volcanoes. [PDF]
Zhao L+8 more
europepmc +1 more source