Results 171 to 180 of about 45,915 (265)
Abstract Long‐term rates of crustal uplift in southern Calabria and NE Sicily are incompletely understood due to limited information about the age of marine terraces at 1.0–1.3 km above sea level (asl). This study provides a new constraint on high‐elevation terrace ages through integrated analysis of geochronology, stratigraphy, shoreline modeling, and
Rebecca J. Dorsey +5 more
wiley +1 more source
Abstract In the Central Alps, the Adula unit exposes high‐ and ultra‐high‐pressure (HP‐UHP) metamorphic rocks, providing key insights into the subduction and exhumation dynamics of the former distal European margin. We investigate the San Bernardino Shear Zone (SBSZ), a top‐to‐the‐east extensional shear zone developed within orthogneiss and paragneiss ...
C. Montemagni +4 more
wiley +1 more source
Contemporaneous mobile- and stagnant-lid tectonics on the Hadean Earth. [PDF]
Valley JW +11 more
europepmc +1 more source
Abstract Understanding how spatially variable mountain‐building processes proceed within large intracontinental orogens provides critical insights into continental tectonics and regional paleoenvironmental evolution. Here, we address this issue in the central South Tian Shan (cSTS), a key transitional segment between the well‐studied eastern and ...
Feng Li +11 more
wiley +1 more source
Depth of slab breakoff in Archean: the role of radiogenic heat production of continental crust and eclogitization of oceanic crust. [PDF]
Fan YL, Zhang LF, Wang Y, Li ZH.
europepmc +1 more source
Abstract An updated approach to seismically constrained modeling of gravity data reveals two broad, NW‐trending low‐density zones in the mantle lithosphere beneath the Canadian Cordillera. The low‐density zones coincide with a shallow lithosphere‐asthenosphere boundary (LAB), a shallow Curie‐point depth, and the location of Quaternary volcanoes.
Nathan Hayward, Tark S. Hamilton
wiley +1 more source
The mantle source of REE-rich alkaline silicate magmas can be enriched by continent-derived sediment subduction. [PDF]
Qiu KF +8 more
europepmc +1 more source
The Impact of Orogenic Inheritance on Rifted Margin Formation
Abstract Many rifted margins form within pre‐existing orogenic belts, emphasizing the significance of structural, thermal, and compositional inheritance in shaping rift dynamics. However, a key unresolved question is how these different types of orogenic inheritance individually influence rift evolution.
Kai Li +4 more
wiley +1 more source
Delineating the Central Anatolia Transition Zone (CATZ): Constraints from Integrated Geodetic (GNSS/InSAR) and Seismic Data. [PDF]
Kutoğlu ŞH, Akgün E, Softa M.
europepmc +1 more source
Abstract Recent earthquakes along the shallow portion of the Hikurangi subduction zone (the 2016 Kaikoura earthquake sequence, New Zealand) indicate that faults within the overriding plate of subduction zones may exhibit uncharacteristically large surface displacements relative to their fault length. Whether this style of upper‐plate faulting is common
K. A. McKenzie +3 more
wiley +1 more source

