Much of the Earth's mantle was melted in the Moon-forming impact. Gases that were not
partially soluble in the melt, such as water and CO2, formed a thick, deep atmosphere …

The global mid-ocean ridge is segmented in its seafloor morphology and magmatic systems,
but the origin of and relationships between this tectonic and magmatic segmentation are …

Traditionally, stellar radiation has been the only heat source considered capable of
determining global climate on long timescales. Here, we show that terrestrial exoplanets …

The thermal state of mid-ocean ridges exerts a crucial modulation on seafloor spreading
processes that shape~ 2/3 of our planet's surface. Standard thermal models treat the ridge …

Detailed images of the midcrustal magmatic system beneath the East Pacific Rise (8° 20′–
10° 10′ N) are obtained from 2‐D and 3‐D‐swath processing of along axis seismic data …

Melt supply at slow‐ultraslow spreading ridges is overall reduced and highly variable.
Magma cooling and crystallization substantially shape the axial thermal regime by providing …

Oceanic crustal accretion at mid-ocean ridges is a function of spreading rate, mantle
temperature, and composition, which are intertwined in affecting melt production and …

We have reviewed available visual information from the seafloor, and recently acquired
microbathymetry for several traverses across the Lucky Strike segment, to evaluate the …

We use three‐dimensional multistreamer seismic reflection data to investigate variations in
axial magma lens (AML) physical properties along the East Pacific Rise between 9° 30′ N …

We apply wave equation‐based techniques to 2‐D seismic data to characterize the nature of
zero‐age upper crust at the East Pacific Rise from 9° 16′ to 9° 56′ N. The final velocity …