Results 191 to 200 of about 22,424 (265)
Illuminating subduction zone rheological properties in the wake of a giant earthquake. [PDF]
Weiss JR +16 more
europepmc +1 more source
Nishinoshima is a volcanic island in the Ogasawara Arc that has exhibited intermittent activity since 2013, including four major eruptive episodes: 2013–2015 (Episode 1), 2017 (Episode 2), 2018 (Episode 3), and 2019–2020 (Episode 4). Previous studies reported a change in eruption style—from a Strombolian eruption with lava flows (Episode 1 to the early
Erika Tanaka +4 more
wiley +1 more source
Sulphur and carbon cycling in the subduction zone mélange. [PDF]
Schwarzenbach EM +5 more
europepmc +1 more source
Mordenite is a naturally occurring zeolite mineral that is the seventh most common zeolite mineral globally, forming at low temperatures (≥100°C) in hydrothermal systems. In New Zealand, extensive deposits of mordenite are commonly associated with areas of hydrothermal alteration, particularly in the Coromandel and Taupo Volcanic Zones.
Ayrton R. Hamilton +6 more
wiley +1 more source
Low Hazard–High Risk: A Case Study of the Active Mangatangi Fault
Activity on low deformation rate faults are challenging to quantify and comparatively understudied. One such fault, the Mangatangi Fault, strikes NE‐SW along the southeastern flanks of the Hunua Ranges c. 52 km south of New Zealand's most populous city, Auckland.
Hannah E. Martin +3 more
wiley +1 more source
The Milun Fault forms the northernmost onshore segment of the Longitudinal Valley fault system, a plate‐boundary suture between the Eurasian and Philippine Sea plates in eastern Taiwan, and poses a significant seismic hazard to Hualien City. Despite destructive earthquakes in 1951 and 2018, the shallow structure, long‐term slip behavior, and ...
Wen‐Jeng Huang +6 more
wiley +1 more source
Earthquake swarms and slow slip on a sliver fault in the Mexican subduction zone. [PDF]
Fasola SL +4 more
europepmc +1 more source
Abstract The turnover rate of microbial cells drops steeply by increasing depth in the seabed, in accordance with the decreasing rate of organic matter mineralization. Bacterial endospore formation and germination may take place concurrently, yet their coupling to the mineralization rates during burial is poorly understood.
Bo Barker Jørgensen +6 more
wiley +1 more source
Crustal Structure of the Collision-Subduction Zone in South of Iran Using Virtual Seismometers. [PDF]
Shirzad T, Riahi MA, Assumpção MS.
europepmc +1 more source
A global assessment of abyssal–hadal vermiform lebensspuren: Functional consistency with depth
Abstract Lebensspuren—sedimentary traces produced by benthic organisms—are widespread on deep‐sea floors but remain infrequently reported from abyssal (~ 3000–6000) and hadal (> 6000 m) environments. Here, we present the most comprehensive assessment of abyssal–hadal vermiform lebensspuren to date, spanning multiple ocean basins and reaching full‐ocean
Denise J. B. Swanborn +2 more
wiley +1 more source

