Results 91 to 100 of about 5,763 (231)
This study presents the synthesis and ball-milling modification of titanite (CaTiSiO5) powders to enhance the thermal stability and performance of polypropylene (PP) separators for lithium-ion batteries (LIBs).
Mirza Mariela Ruiz-Ramirez +6 more
doaj +1 more source
Rutile and titanite commonly form by replacement of ilmenite in metamorphic rocks. Exhumed orthogneiss from the Western Alps show that titanite is mostly stable below 1 GPa while rutile seems to dominate within rocks recrystallized under higher pressures.
S. Angiboust, D. Harlov
semanticscholar +1 more source
The article reports on the presence of minerals of the crichtonite group (MCG) in ooids of mineralized volcaniclastic rocks of the Rudnogorskoe iron deposit (Eastern Siberia).
Nuriya R. Ayupova +4 more
doaj
The subduction interface hosts megathrust earthquakes and ductile creep, is fluid‐rich and chemically dynamic, and produces metasomatic rocks that may host episodic tremor and slow slip (ETS).
W. Hoover +5 more
doaj +1 more source
High-Pressure Marbles from the Nahavand Area in the Sanandaj-Sirjan Metamorphic Belt, Iran [PDF]
Marbles containing high-pressure mineral assemblage was found from the Sanandaj-Sirjan metamorphic belt in the Nahavand area in western Iran. The high-pressure marbles occur as small bodies or lenses within pelitic schist layers and show compositional ...
J. Izadyar, N. Skandari
doaj
Emplacement of the Argyle diamond deposit into an ancient rift zone triggered by supercontinent breakup. [PDF]
Olierook HKH +14 more
europepmc +1 more source
Synthesis of Ilmenite Nickel Titanite-Supported Carbon Nanofibers Derived from Polyvinylpyrrolidone as Photocatalyst for H2 Production from Ammonia Borane Photohydrolysis. [PDF]
Maafa IM +7 more
europepmc +1 more source
Magmatic surge requires two-stage model for the Laramide orogeny. [PDF]
Schwartz JJ +6 more
europepmc +1 more source
Cryptic geological histories accessed through entombed and matrix geochronometers in dykes
Deep geology of ancient continental crust can be difficult to access, with direct observation restricted to limited exposures. The age and composition of hidden geology can be gleaned from indirect isotopic modelling or via detrital minerals within ...
Christopher L. Kirkland +9 more
doaj +1 more source

