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Geologists discover evidence of gas hydrates in the Manila Trench

Geologists discover evidence of gas hydrates in the Manila Trench
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Another large earthquake strikes the southern Philippines

The magnitude-7.3 earthquake that struck off the coast of Mindanao, Philippines, this week could have inflicted heavy damage had the quake been shallow and onshore.

Latest Philippine earthquake reveals tectonic complexity

Latest Philippine earthquake reveals tectonic complexity Posted on   Mario Aurelio, Director of the University of the Philippines National Institute of Geological Sciences, Mahar Lagmay, Executive Director, University of the Philippines Resilience Institute-Nationwide Operational Assessment of Hazards Center (@nababaha), John Agustin Escudero, Structural Geology and Tectonics Laboratory at the University of Philippines National Institute of Geological Sciences, Sandra Catugas, Structural Geology and Tectonics Laboratory at the University of Philippines National Institute of Geological Sciences   Citation: Aurelio, M., Lagmay, M., Escudero, J. A., and Catugas, S., 2021, Latest Philippine earthquake reveals tectonic complexity, Temblor, http://doi.org/10.32858/temblor.191   A magnitude-6.6 earthquake struck the island of Luzon, Philippines, at 4:47 a.m. local time on Saturday, July 24 (data from the Philippine Institute of Volcanology and Seismology, or PHIVOLCS). T

GSA Bulletin articles published ahead of print in January

Emilia A. Caylor; Barbara Carrapa; Kurt Sundell; Peter G. DeCelles; Joshua M. Smith Abstract: The Upper Cretaceous Fort Crittenden Formation exposed in the Santa Rita and Huachuca Mountains of southeastern Arizona is a syntectonic deposit that has been associated with Laramide tectonic activity. However, the spatio-temporal relationships among Cretaceous sedimentation, magmatism, basement exhumation, and possible flat slab-related processes in the southern Laramide region remain poorly understood. Age controls for uplift and erosion of local topography and syntectonic deposition in response to deformation remain particularly poor. The Fort Crittenden Formation comprises 800?2500 m of locally derived fluvial to alluvial fan sedimentary rocks and records paleodrainage reorganization in response to active tectonics. Changes in sedimentary facies, provenance, and paleoflow suggest deposition in a tectonically partitioned intraforeland basin. New detrital zircon data constrain the timin

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