Layered intrusions: Fundamentals, novel observations and concepts, and controversial issues
Layered intrusions are fossilized natural laboratories that historically have constrained many
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …
The diverse planetary ingassing/outgassing paths produced over billions of years of magmatic activity
The CHONS elements that constitute the outgassed atmosphere and exosphere have likely
been delivered by chondritic materials to the Earth during planetary accretion and …
been delivered by chondritic materials to the Earth during planetary accretion and …
Redox controls during magma ocean degassing
Nitrogen, carbon, hydrogen and sulfur are essential elements for life and comprise about 1%
of terrestrial planet masses. These elements dominate planetary surfaces due to their …
of terrestrial planet masses. These elements dominate planetary surfaces due to their …
A theoretical framework for volcanic degassing chemistry in a comparative planetology perspective and implications for planetary atmospheres
F Gaillard, B Scaillet - Earth and Planetary Science Letters, 2014 - Elsevier
Magmatic degassing is ubiquitous and enduring, yet its impact on both planetary surficial
chemistry and how it may have varied among planetary systems remains imprecise. A large …
chemistry and how it may have varied among planetary systems remains imprecise. A large …
Geo‐fO2: Integrated Software for Analysis of Magmatic Oxygen Fugacity
W Li, Y Cheng, Z Yang - Geochemistry, Geophysics …, 2019 - Wiley Online Library
Oxygen fugacity (fO2) is a fundamental thermodynamic property governing redox potential in
solid Earth systems. Analysis of magmatic fO2 aids our understanding of the valence state …
solid Earth systems. Analysis of magmatic fO2 aids our understanding of the valence state …
The effects of large igneous provinces on the global carbon and sulphur cycles
The correlation between large igneous provinces (LIPs), extinction events, and rapid climate
change suggests that volcanism can have a detrimental impact on Earth surface conditions …
change suggests that volcanism can have a detrimental impact on Earth surface conditions …
The redox geodynamics linking basalts and their mantle sources through space and time
F Gaillard, B Scaillet, M Pichavant, G Iacono-Marziano - Chemical Geology, 2015 - Elsevier
The Earth's mantle redox state regulates the fate and transfer of metals by magmatism,
buffers the igneous inputs of volcanic gases in the atmosphere and controls the depth of …
buffers the igneous inputs of volcanic gases in the atmosphere and controls the depth of …
Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province
Exceptional magmatic events coincided with the largest mass extinctions throughout Earth's
history. Extensive degassing from organic-rich sediments intruded by magmas is a possible …
history. Extensive degassing from organic-rich sediments intruded by magmas is a possible …
Orbital multispectral mapping of Mercury with the MESSENGER Mercury Dual Imaging System: Evidence for the origins of plains units and low-reflectance material
A principal data product from MESSENGER's primary orbital mission at Mercury is a global
multispectral map in eight visible to near-infrared colors, at an average pixel scale of 1 km …
multispectral map in eight visible to near-infrared colors, at an average pixel scale of 1 km …
Magma–shale interaction in large igneous provinces: implications for climate warming and sulfide genesis
Large igneous provinces (LIPs) whose magma plumbing systems intersect sedimentary
basins are linked to upheavals of Earth's carbon and sulfur cycles and thus climate and life …
basins are linked to upheavals of Earth's carbon and sulfur cycles and thus climate and life …