3D numerical simulation-based targeting of skarn type mineralization within the Xuancheng-Magushan orefield, middle-lower Yangtze metallogenic belt, China
Recent exploration has identified a series of Cu-Mo skarn deposits within the Xuancheng-
Magushan orefield. The orefield forms part of the Nanling-Xuancheng mining district, which …
Magushan orefield. The orefield forms part of the Nanling-Xuancheng mining district, which …
Systematic characterization of morphotectonic variability along the Cascadia convergent margin: Implications for shallow megathrust behavior and tsunami hazards
JT Watt, DS Brothers - Geosphere, 2021 - pubs.geoscienceworld.org
Studies of recent destructive megathrust earthquakes and tsunamis along subduction
margins in Japan, Sumatra, and Chile have linked forearc morphology and structure to …
margins in Japan, Sumatra, and Chile have linked forearc morphology and structure to …
[HTML][HTML] Understanding partitioning of deformation in highly arcuate orogenic systems: Inferences from the evolution of the Serbian Carpathians
Highly curved orogens often demonstrate a complex poly-phase tectonic evolution and
significant strain partitioning. While the oroclinal bending towards the outer arc is …
significant strain partitioning. While the oroclinal bending towards the outer arc is …
Subducting plate structure and megathrust morphology from deep seismic imaging linked to earthquake rupture segmentation at Cascadia
The origin of rupture segmentation along subduction zone megathrusts and linkages to the
structural evolution of the subduction zone are poorly understood. Here, regional-scale …
structural evolution of the subduction zone are poorly understood. Here, regional-scale …
Discovery of an Active Forearc Fault in an Urban Region: Holocene Rupture on the X EOL X ELE K‐Elk Lake Fault, Victoria, British Columbia, Canada
Subduction forearcs are subject to seismic hazard from upper plate faults that are often
invisible to instrumental monitoring networks. Identifying active faults in forearcs therefore …
invisible to instrumental monitoring networks. Identifying active faults in forearcs therefore …
100 myr cycles of oceanic lithosphere generation in peri-Gondwana: Neoproterozoic–Devonian ophiolites from the NW African–Iberian margin of Gondwana and the …
Abstract The Variscan Orogen in Iberia and the Anti-Atlas Mountains in Morocco contains a
set of ophiolites formed between Neoproterozoic and Devonian times, during the complex …
set of ophiolites formed between Neoproterozoic and Devonian times, during the complex …
[HTML][HTML] Exhumation response to oceanic plateau accretion and oroclinal bending: Low-temperature thermochronology study of Wrangellia terrane on southern …
Approximately 50 Myr ago, the triple junction of the Kula-Farallon-North America plates
converged with the continental margin, causing ridge subduction and the formation …
converged with the continental margin, causing ridge subduction and the formation …
Paleoseismic trenching reveals Late Quaternary kinematics of the Leech River fault: Implications for forearc strain accumulation in northern Cascadia
N Harrichhausen, KD Morell… - Bulletin of the …, 2021 - pubs.geoscienceworld.org
New paleoseismic trenching indicates late Quaternary oblique right‐lateral slip on the Leech
River fault, southern Vancouver Island, Canada, and constrains permanent forearc …
River fault, southern Vancouver Island, Canada, and constrains permanent forearc …
[HTML][HTML] The fate of marine magnetic anomaly in subduction zones: A global appraisal
H Choe, J Dyment - Earth and Planetary Science Letters, 2021 - Elsevier
Seafloor spreading magnetic anomalies of oceanic plates progressively decay and
disappear when approaching and entering subduction. Previous studies focused on the …
disappear when approaching and entering subduction. Previous studies focused on the …
Late middle Miocene emergence of the Olympic Peninsula shown by sedimentary provenance
Abstract The Olympic Peninsula is the uplifted portion of the Cascadia accretionary wedge
and forms the core of a 200 km scale oroclinal bend on the west coast of Washington State …
and forms the core of a 200 km scale oroclinal bend on the west coast of Washington State …