Seismic catalog reveals forearc activity and slab dip variations. Vp anomalies in the oceanic plate are related to mid-depth seismic events

Velocity models uncover anomalies in Salar de Atacama and Taltal ridge that might influence seismicity distribution and hydration changes

Shallow low Vp/Vs (<1.75) correlate with ore deposits; deep high Vp/Vs (>1.80) suggest fluids and melting for the Lastarria volcanic complex

Stalagmites record past fire activity through changes in inorganic and organic chemistry sourced from ashes

Wildfire ash leachate chemistry will aid interpretation of proxy fire data

Results show that inorganic chemistry varies with burn severity and sample location, and the pyrogenic biomarker signal is less clear

Natural hydrogen exploration in former oil and gas province

Use of the Optical Character Recognition algorithm to optimize processing of a large drilling report database

Indices for a potential H₂ system (source, migration, trap) in the Paris Basin

S isotopic variations caused by Rayleigh fractionation between sulphide and reduced S; Cd isotopic variations inherited from source rocks

Zn/Cd ratios and Cd isotopic compositions reveal that Zn and Cd were dominantly derived from basement rocks

The Nayongzhi deposit was formed by mixing between metal-rich and reduced sulfur ore-forming fluids

The mobility of mattes is enhanced by majoritic garnet at sub-lithospheric depths

The combination of 2D and 3D methods improves our understanding of liquid percolation in the Earth's mantle

New dating indicates that a major part of the oldest Philippine Sea Plate basins formed after c. 51 Ma

Ocean crust of the oldest Philippine Basins is affected by the Oki-Daito mantle plume

Onset of spreading of the West Philippine Basin could have been triggered when the Oki-Daito plume hit the base of preexisting lithosphere

During Neo-Tethyan subduction, pyroxenite-bearing domains formed by melt intrusion into the lower lithosphere beneath Eastern Anatolia

The pyroxenite-bearing domains resulted in gravitational instabilities and led to the foundering of the lithosphere in the Late Miocene

The regional post-collisional volcanics represent the melts derived both from asthenospheric and delaminated lithospheric mantle domains

Archaeomagnetic intensity data from 32 groups of pottery in Israel dated between the 7th and the 1st centuries BCE

The second generation of the Levantine Archaeomagnetic Curve (LAC.v.2.0) covering the last three millennia BCE

The new data constrain the duration of the Levantine Iron Age Anomaly (LIAA) from 1100 BCE to 550 BCE

Maximum eruptible S contents (ppm S) are estimated for 73 Icelandic eruptions based on melt inclusion data

Pre-eruptive S contents are mostly controlled by sulfide saturation during both melting and crustal magmatic differentiation

Icelandic basalts often erupt at compositions close to a compositional maximum in sulfide solubility, leading to relatively high S emissions