Results 61 to 70 of about 2,496,797 (168)

Fast and Spatially Heterogeneous Cooling Rates at Amphibolite‐Facies Conditions in the Lepontine Alps (Switzerland)

open access: yesGeochemistry, Geophysics, Geosystems, Volume 26, Issue 11, November 2025.
Abstract The Lepontine dome (European Central Alps) is constituted by basement nappes under Alpine regional Barrovian metamorphism, yet the duration and pattern of its post‐peak amphibolite‐facies cooling remain uncertain. We examine garnet‐rim compositional re‐adjustment and employ inverse multicomponent diffusion modeling to estimate apparent cooling
A. Tagliaferri   +3 more
wiley   +1 more source

Allanite-(Ce) and rare earth element bearing epidotes in the albitites of central Sardinia (Italy)|Allanite-(Ce) ed epidoti a Terre Rare nelle albititi della Sardegna centrale (Italia)

open access: yes, 1996
Recent investigations have pointed out that epidotes and allanite-(Ce) are the main REE-bearing minerals in the albitites located in the granodiorite facies of Central Sardinia.
Tamanini M, Carcangiu G, Palomba M
core  

Unusual LREE-rich, peraluminous, monazite- or allanite-bearing pegmatitic granite in the central Grenville Province, Québec

open access: yes, 2017
International audienceThis contribution presents an original study combining detailed mapping, petrography, whole-rock geochemistry and geochronological constraints on the recently identified LREE (Light Rare Earth Elements) occurrences associated with ...
Gervais, Félix   +15 more
core   +1 more source

Apatite-hosted REE mineralization in the Eastern Ghats Mobile Belt: A future prospect for REE

open access: yesGeosystems and Geoenvironment
The growing need of rare earth elements in different sectors of the modern-day world has led to their increasing demand, which is in accordance with their limited supply.
Mousumi Bhattacharjee   +2 more
doaj   +1 more source

Tonian shoshonitic to ultrapotassic granitoids from Chhotanagpur Gneissic Complex, Eastern Indian Shield: Age, origin and tectonic implications

open access: yesGeosystems and Geoenvironment
This work reports petrogenesis of an ultrapotassic granitoid pluton emplaced in the Tonian (949.4 ± 2.3 Ma; new LA-ICPMS zircon U–Pb dating) along a regional shear zone during the post-collisional stage of the Grenvillian Satpura orogeny in Eastern India.
Ankita Basak   +4 more
doaj   +1 more source

Non-matrix-matched standardisation in LA-ICP-MS analysis: general approach, and application to allanite Th–U–Pb dating [PDF]

open access: yes, 2017
To make use of the full geochronological potential of accessory minerals such as zircon, allanite, monazite, and titanite, high spatial resolution isotopic analysis of the Th–U–Pb system is required.
Pettke, Thomas   +7 more
core   +1 more source

Redistribution of REE, Y, Th, and U at high pressure: Allanite-forming reactions in impure meta-quartzites (Sesia Zone, Western Italian Alps)

open access: yes, 2012
International audienceAccessory phases are important hosts of trace elements; allanite may contain >90% of the REE in a bulk rock. The mobility and redistribution of several trace elements, notably HREE, Th, U, and Y is thus controlled by reactions ...
Cenki-Tok, B.   +7 more
core   +1 more source

Why allanite may swindle about its true age

open access: yes, 2003
Allanite from the Tertiary Rieserferner pluton (Austrian Alps) is texturally and chemically heterogeneous. Continuous covariation trends reflect coupled substitution of Ca+Al vs.
Siegesmund, Siegfried, Romer, Rolf L.
core   +1 more source

Rare earth element evolution and migration in plagiogranites: a record preserved in epidote and allanite of the Troodos ophiolite

open access: yes, 2015
Plagiogranites from the Troodos ophiolite in Cyprus are occasionally epidotised, either partially or completely. Epidotisation phenomena include replacement of pre-existing minerals and filling of miarolitic cavities.
Bach, Wolfgang   +4 more
core   +1 more source

Chemical properties of allanite from the Ryoke and Hirosima granite pegmatites in Shikoku, Japan

open access: yes, 2001
Allanite is one of the most common REE minerals in the Ryoke and Hiroshima granite pegmatites. It generally occurs as prismatic crystal up to 20cm in length to tabular masses in the contact zone of ferro-biotite and feldspar.
船越, 議生   +2 more
core  

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