Results 71 to 80 of about 2,520 (206)
A record of magmatic differentiation in plutonic xenoliths from Santorini (Greece)
Plutonic xenoliths from volcanic arcs provide unique insights into transcrustal magmatic systems in subduction zone settings. At Santorini volcano in the Central Aegean Volcanic Arc (Greece), plutonic xenoliths occur throughout a sequence of lavas and ...
Sean Whitley +5 more
doaj +1 more source
Allanite in Mantle Eclogite Xenoliths
Abstract Rare-Earth Elements (REE) are key geochemical tracers of crust–mantle differentiation, but there are few direct data on REE-rich minerals in mantle rocks. Here, we report the combined petrography and comprehensive chemical and isotopic characterization of three coesite- and kyanite-bearing eclogite xenoliths from the Udachnaya ...
Denis S Mikhailenko +5 more
openaire +1 more source
Syn-volcanic melt-rock reactions recorded in peridotitic xenoliths from Scania, S Sweden
Peridotite xenoliths from Scania (S Sweden), brought to the surface by Mesozoic basanitic magmas, provide insights into the lithospheric mantle underlying the East European Craton.
Kukuła Anna +4 more
doaj +1 more source
[Artikel-Nr.: 108156] Sheared garnet peridotites occur in the deep lithosphere and record processes of deformation, melt interaction, and metasomatism along the lithosphere-asthenosphere boundary (LAB).
Bussweiler, Yannick +5 more
core +1 more source
Mineral analyses and reconstructed bulk xenolith compositions for the Kaapvaal craton
EPMA & LA-ICP-MS mineral analyses and reconstructed bulk xenolith compositionsTHIS DATASET IS ARCHIVED AT DANS/EASY, BUT NOT ACCESSIBLE HERE.
Gibson, S (via Mendeley Data)
core +1 more source
Sub-Zero Alteration in an Isotopically Heavy Brine Preserved in a Pristine H Chondrite Xenolith [PDF]
Introduction: Brecciated H chondrites host a variety of xenoliths, including unshocked, phyllo- silicate-rich carbonaceous chondrites (CCs). The brecciated H chondrite Zag (H3-6) is one of two chondrites to host macroscopic (1 - 5mm), xenolithic crystals
Zolensky, M. E. +3 more
core
How Cratonic Roots Survive With Weak Mid‐Lithosphere Discontinuities
The stability of cratons has long been attributed to their neutral buoyancy and strong roots. However, recent seismic studies have revealed widespread mid‐lithospheric discontinuities (MLDs) within cratonic roots.
Qionghua Guo, Huilin Wang, Honglei Liu
doaj +1 more source
Modes of Occurrence of Spinel in Xenoliths.,
During his petrological study on the inclusions in the garnet-biotite-andesite from Nijo Volcano near Osaka, the present writer pointed out the common occurrence of spinel associating intimately with porphyroblastic andalusite or sillimanite in some xenoliths derived from argillaceous metamorphic rock, as the feature to be observed in xenoliths when ...
openaire +2 more sources
Mantle-derived peridotite xenoliths represent a valuable source of information about the structure, chemistry, origin, and evolution of the mantle lithosphere underlying various tectonic environments. Xenolith-bearing volcanic suites at Mt.
Kroner, Ryan Keith
core +1 more source
Karst phenomena, such as fissures and caves, occur in the marble agglomerate of pyroclastic rocks on the eastern slope of Shenzhen’s Wutong Mountain. These features have affected the engineering projects such as subway construction and pile foundation ...
Xiaohu WANG +3 more
doaj +1 more source

