Results 91 to 100 of about 9,495 (248)
The chemical makeup of Earth’s atmosphere during the Archean (4–2.5 Ga) and Proterozoic eon (2.5–0.5 Ga) contrast considerably with the present-day: the Archean was rich in carbon dioxide and methane, and the Proterozoic had potentially higher amounts of
Armen Tokadjian, Renyu Hu, Mario Damiano
doaj +1 more source
Multi‐Scale Electrical Conductivity Model of the Contiguous United States
Abstract The completion of the Magnetotelluric (MT) USArray across the contiguous US enables continental‐scale 3‐D imaging of the asthenosphere‐lithosphere electrical structure. We present a novel 3‐D model of the contiguous United States (MECMUS), derived from a single inversion of the now‐completed USMTArray data set.
Federico D. Munch, Alexander Grayver
wiley +1 more source
Secular Changes in the Occurrence of Subduction During the Archean
Subduction processes play a pivotal role in facilitating material exchange between the crust and mantle, contributing to the growth of continents. However, the onset and evolution of subduction remain hotly debated.
Chun‐Tao Liu +2 more
doaj +1 more source
The karst geothermal reservoir in Xiong'an New Area is a representative example of an ancient buried hill geothermal system. However, published heat flow data are predominantly derived from the Cenozoic sedimentary cap.
Ya-hui Yao +7 more
doaj +1 more source
Data‐Driven Investigation Reveals Subaerial Proportion of Basalts Since the Early Archean
The subaerial exposure of the modern continental crust through time remains intensely debated, with estimates of the first exposure ranging from the late Archean to the Neoproterozoic.
Chun‐Tao Liu +2 more
doaj +1 more source
Was H2O2 generated before oxygenic photosynthesis?
We obviously agree with Wu et al. that H2O2 might accumulate in the Archean land waters devoid of Fe2+. We do disagree on the topic of the half-life of H2O2, as the work cited in support for a longer half-live is not relevant to the conditions in the ...
Willem H. Koppenol, Helmut Sies
doaj +1 more source
Geochemistry and petrogenesis of Archean mafic and ultramafic rocks, Southern West Greenland
Frances E. Jenner
openalex +1 more source
Around 80% of the world’s hard-rock lithium supply comes from pegmatites formed in the Archean Eon, yet our understanding of how Lithium-pegmatites form assumes magma source compositions not relevant to those Archean cratons hosting most of the giant ...
Robert H. Smithies +11 more
doaj +1 more source
Geological Evidence for the Operation of Plate Tectonics throughout the Archean: Records from Archean Paleo-Plate Boundaries [PDF]
Timothy Kusky +2 more
openalex +1 more source

