Browse Articles

New insights into the geology and formation of the Araguainha impact structure, Brazil, from morphological and structural analysis

Optimizing methods for Raman spectroscopy of carbonaceous material thermometry: Best practices to develop high-fidelity thermal constraints for tectonic studies

Transform fault system: A microplate-based perspective on transform faults

The role of mantle melting and associated granitoid magmatism in the genesis of orogenic gold in the Laurentian Caledonides

Microstructural and geochemical response of muscovite to impact metamorphism

Chemosynthetic microbial communities formed wrinkle structures in ancient turbidites

The driving of the Yigong earthquake swarm and the seasonal variations

Structural framework, protolith affinity, and <i>P-T-t-D</i> evolution of the metasediments exposed in the Lalong dome, eastern Himalaya: Evidence of the upper South Tibetan detachment system in the northern Himalaya

Mantle-driven, climatically modulated landscape evolution in Southern Patagonia

Xenolith hydrogen isotope evidence for lower crustal hydration during cycles of flat slab subduction

Seafloor weathering can explain the disparate durations of Snowball glaciations

Geraisite: The first tektite occurrence in Brazil

Empowered by Opportunity: My First GSA Connects Experience Through the OTF Program

I am Khadijah Audu, a PhD student in the geosciences at the University of Arkansas, where I specialize in remote sensing...

SWOT Satellite: A New Tool for Fluvial Geomorphology

Earth-observing satellites have revolutionized the field of fluvial geomorphology by providing large-scale and spatially...

Incorporating Ethics in College Geoscience Education through Community Engagement

Department of Earth and Environmental Sciences, Indiana University Indianapolis, Indianapolis, Indiana 46202, USA

Vestiges of Earth's earliest depleted mantle reservoir: REPLY

Vestiges of Earth's earliest depleted mantle reservoir: COMMENT

Intraplate volcanism induced by magmatic solitary waves ascending from the mantle transition zone