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Showing 1–4 of 4 results

Advanced filters: Author: Matthew Steele-MacInnis Clear advanced filters

Correction: Corrigendum: Seismic precursors linked to highly compressible fluids at oceanic transform faults

Louis Géli
Jean-Michel Piau
Thomas Driesner
Amendments and Corrections24 Dec 2015
Nature Geoscience

Volume: 9, P: 83
Seismic precursors linked to highly compressible fluids at oceanic transform faults

Earthquakes on oceanic transform faults are often preceded by foreshock swarms. A theoretical model suggests that circulating hydrothermal fluids, which compress as the fault rocks expand and deform, cause this precursor seismic activity.

Louis Géli
Jean-Michel Piau
Thomas Driesner
Research14 Sept 2014
Nature Geoscience

Volume: 7, P: 757-761
Magmatic immiscibility and the origin of magnetite-(apatite) iron deposits

Magnetite-apatite (MtAp) deposits are an important source of iron and critical metals, yet their ore genesis is poorly understood. Here, authors propose that the separation of multiple melts during magma ascent leads to the formation of MtAp deposits.

Dorota K. Pietruszka
John M. Hanchar
Wyatt M. Bain
ResearchOpen Access19 Dec 2023
Nature Communications

Volume: 14, P: 1-11
A fundamental role of carbonate–sulfate melts in the formation of iron oxide–apatite deposits

Iron-rich carbonate–sulfate melts are fundamental to the formation of iron oxide–apatite ore deposits, according to a detailed fluid-inclusion study that characterized the mineralizing fluids for two mineralizing systems in the United States.

Wyatt M. Bain
Matthew Steele-MacInnis
Erin E. Marsh
Research21 Sept 2020
Nature Geoscience

Volume: 13, P: 751-757