Results 81 to 90 of about 5,325 (163)
Troodos: A Giant Serpentinite Diapir
Troodos is a classical ophiolite complex. It is proposed that the serpentinized harzburgites that now form the top of the mountain and represent the originally lowest part of the ophiolite sequence rose as a diapir. This diapiric rise is caused by the pervasive serpentinization of a suboceanic harzburgite, due to rock-sea water interaction.
openaire +3 more sources
Accessory Minerals in New Idria serpentinite
Serpentinite is a rock composed almost wholly of serpentine-group minerals and contain accessory minerals that are sensitive to formation chemical condition. In 2017 Patton did a study on accessory minerals of an ophiolite.
Murrey, Michael
core +6 more sources
Abstract Same‐dip double subduction (SDDS), in which two parallel slabs dip in the same direction, has been linked to accelerated plate motion in both modern and ancient convergent systems, such as the Late Cretaceous Africa–Eurasia system. Yet a systematic framework for quantifying how SDDS alters plate kinematics in a large‐scale spherical geometry ...
Zonglin Guo, Adam F. Holt, Derya Gürer
wiley +1 more source
Abstract Magnesite (MgCO3) is a magnesium (Mg) carbonate mineral that records the aqueous environmental conditions of its formation. On Earth, magnesite forms in metamorphic, diagenetic or pedogenic environments, and distinguishing between these environments is critical for understanding the fluid chemistry during magnesite precipitation. Mg carbonates
E. L. Cardarelli +6 more
wiley +1 more source
Abstract We present evidence of a previously unrecognized east‐west‐trending normal fault, named the Parguera Fault, in southwest Puerto Rico. The fault is located at the northwestern edge of seismicity from the southwest Puerto Rico seismic sequence that began in 2019, near the coastal town of La Parguera.
Jessica Thompson Jobe +12 more
wiley +1 more source
Boron isotopes identify deep-slab serpentinite in the source of Aleutian arc magma
Seafloor lavas of the Western Aleutian arc have isotopically heavy boron (delta B-11 to +13.4%(0)) that is negatively correlated with B content (ppm). Endmember samples are primitive dacites and rhyodacites (delta B-11 > +10%(0), SiO2 = 63%-70%, Mg# > 0 ...
Ryan, Jeffrey +7 more
core +1 more source
Petrological review of the Ófalu serpentinite, Mecsek Mountains, Hungary [PDF]
The Ófalu serpentinite as a 10 m thick sill-like body lies in the metamorphites of the Ófalu Group. It consists of two varieties petrographically: ]. massive serpentinite, 2.
Ghoneim Mohamed Ahmed F. +1 more
core
Recycling of heavy noble gases by subduction of serpentinite
Isotopic analyses of natural samples suggest that the heavy noble gases (HNG; Ar, Kr, and Xe) in the mantle are dominated by components recycled by subduction (Holland and Ballentine, 2006, Kendrick et al., 2011, Parai and Mukhopadhyay, 2018, Smye et al.,
Kelley, Simon P. +2 more
core +1 more source
The process of transformation of the silicate components of the crystal lattice structure of chrysotile during its quantitative interaction with aqueous solutions containing various stoichiometrically required amounts of sulfuric acid (SRA H2SO4 ...
Abdrazak Auyeshov +5 more
doaj +1 more source
ABSTRACT The breeding systems of Lutruwita/Tasmania's threatened Epacris taxa are poorly known. Our main objective was to determine the pollinators of several endemic species and explore for relationships between pollinators, floral morphology, flowering time and habitat. The Epacris have limited variation in floral traits and exhibit generalist floral
Karen A. Johnson, Peter B. McQuillan
wiley +1 more source

