«Our work offers new tools to constrain the physical and chemical conditions in the mantle responsible
for large igneous provinces,» Brown said.
Not exact matches
Based on the volcanic record in and around Iceland over the last 56 million years and numerical modeling, Brown and Lesher show that high mantle temperatures are essential
for generating the
large magma volumes that gave rise to the North Atlantic
large igneous provinces bordering Greenland and northern Europe.
At the time when these eruptions took place, 717 million years ago, the Franklin
large igneous province was near the equator, making it easier
for the sulfur dioxide plumes to reach, and cross, the stratosphere and the troposphere.
In Earth's past the trigger
for these greenhouse gas emissions was often unusually massive volcanic eruptions known as «
Large Igneous Provinces,» with knock - on effects that included huge releases of CO2 and methane from organic - rich sediments.