Results 181 to 190 of about 153,348 (348)
ABSTRACT The Ediacaran–Cambrian boundary, which precedes one of the most significant biotic diversification events in Earth's history, is associated with a global negative carbon isotope excursion termed the BAsal Cambrian carbon isotope Excursion (BACE).
Watsawan Chanchai +6 more
wiley +1 more source
Large-scale crustal growth driven by LIP magmatism during the Paleoproterozoic. [PDF]
Simões MS +6 more
europepmc +1 more source
Detrital zircon U-Pb and (U-Th)/He geochronology of the central Morondava Basin, Madagascar
Willem Schetselaar +5 more
openalex +1 more source
A comparison of ceramic and carbon‐based reductants for vitrification of low‐activity waste
Abstract Sucrose is the current baseline additive at the Hanford Waste Treatment and Immobilization Plant in Washington to control foaming during waste feed to glass transitions and the redox state of the glass melt. Alternative reductants are being investigated to alleviate strain on effluent treatment from toxic acetonitrile production from ...
Jessica Rigby +10 more
wiley +1 more source
Linking mineral chemistry and radiological risk in rare-metal-bearing monzogranite in Egypt. [PDF]
Ghoneim MM.
europepmc +1 more source
Assembling the world’s type shallow subduction complex: Detrital zircon geochronologic constraints on the origin of the Nacimiento block, central California Coast Ranges [PDF]
Alan D. Chapman +6 more
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Abstract The Na+ super ion conductor (NaSICON, Na1+xZr2SixP3‐xO12) is a solid electrolyte well‐known for fast, selective Na+ transport at low temperatures, uniquely enabling sodium‐based batteries. Producing high‐quality NaSICON from solid‐state methods, especially when cost‐effective, potentially hygroscopic precursors are used, is not trivial.
Amanda S. Peretti +8 more
wiley +1 more source
Petrogenesis of Late Permian Mafic Rocks in the Western Guangxi Area, SW China: Implications for the Emeishan Mantle Plume Magmatism. [PDF]
Zhang Y, Zhang Z, Yuan Y.
europepmc +1 more source
ABSTRACT Elevated heat flow associated with mafic magmatism in accretionary orogens has often been proposed as a driving mechanism for (ultra)high‐temperature (UHT) metamorphism and anatexis. The Sancheong–Hadong complex, located in the southern Yeongnam Massif, Korea, consists of a ca.
Yuyoung Lee +3 more
wiley +1 more source

