Results 191 to 200 of about 110,511 (334)
Abstract The tectono‐stratigraphic development of continental basins is critical to an understanding of continental tectonics and the formation of metal deposits. The Neoproterozoic, inter‐cratonic Katangan copper basin of Central Africa records a tectono‐stratigraphic evolution and the generation of potential metal transporting fluid pathways ...
M. C. Daly+3 more
wiley +1 more source
Abstract Rock weathering impacts global nutrient cycles but factoring intrinsic properties of bedrock into weathering models remains a challenge. Here we show that two common tracers of silicate weathering—uranium (U) activity ratios and lithium (Li) isotope ratios of river solutes—inform lithology‐specific modes of landscape denudation.
Evan J. Ramos+2 more
wiley +1 more source
Size evolution of micropyrite from diagenesis to low-grade metamorphism [PDF]
Cnudde, Veerle+5 more
core +1 more source
Petrologic evidence for core sulfur degassing in partially differentiated planetesimals. [PDF]
Wang SZ+5 more
europepmc +1 more source
Chamical characteristics of glaucophanitic regional metamorphism
Yôtâro Seki
openalex +2 more sources
Toward a More Stable Supercontinent Columbia in the Statherian
Abstract During the mid‐Proterozoic, nearly all of Earth's continents collided to form supercontinent Columbia. However, the exact timing of its formation is still debated, with estimates ranging from 1.8 to 1.6 Ga. This period, known as the Statherian, is also debated for its affinity to either the Paleoproterozoic or Mesoproterozoic eras.
Chong Wang+6 more
wiley +1 more source
Thermal buffering-controlled temperature variation between Mg-Al-rich rocks and migmatites. [PDF]
March S, Hand M, Morrissey L, Kelsey D.
europepmc +1 more source
Shock metamorphism of ordinary chondrites
D. Stöffler, K. Keil, S. R.D.
semanticscholar +1 more source