U–Pb Dating of Cambrian Magmatism in the Pinerolo‐Sanfront Unit, Dora‐Maira Massif (Western Alps)
ABSTRACT The Pinerolo‐Sanfront Unit (PSU), the structurally lowest tectonic unit of the Dora‐Maira Massif (Western Alps), has been regarded as a monocyclic unit composed of Permo‐Carboniferous sediments and Permian granitoids that were metamorphosed during the Alpine orogeny.
Francesco De Cesari +6 more
wiley +1 more source
The Study of amphibolites in Bahram Gor area (northwest of Gol-e Gohar mine in Sirjan), with emphasis on mineral paragenesis and whole rock chemical data [PDF]
The study area is located northwest of Gol-e Gohar mine (Bahram Gur Protected Zone) in Sirjan, the Kerman Province, a part of the Sanandaj-Sirjan zone.
Seyyed Hesamaddin Moeinzadeh +2 more
doaj +1 more source
ABSTRACT The Southern Brasília Orogen formed during Western Gondwana's final assembly and comprises nappe systems piled against the São Francisco Craton. We present new rutile U–Pb ages from the lowermost Canastra Group (> 2.2 Ga) and the uppermost Carrancas Group (~560 Ma), integrated with published zircon, monazite, garnet, and mica ages from the ...
Rodrigo Irineu Cerri +7 more
wiley +1 more source
In the current correlation chronostratigraphic scheme of early Precambrian of the Ukrainian Shield, among Neoarchean supra crystalline formations of the Buzko-Rosynskyi block, it is identified the Rosynsko-Tikytska series, which consist of the Myzynivska
V. P. Bezvynnyi, M. M. Kostenko
doaj +1 more source
Experimental Evidence for a Weak Calcic‐Amphibole‐Rich Deep Crust in Orogens
Amphibole‐rich rocks constitute significant components of the mid‐ to lower continental crust, particularly in active orogens characterized with thick and hot crusts. Nevertheless, experimental data on their viscosity remain scarce.
X. Wang +7 more
doaj +1 more source
Tectonics on Early Earth Driven by Earth's Changing Shape During Tidal Recession of the Moon
Abstract Few fragments of Earth's earliest crust have survived, and so this formative period of our planet's history is shrouded in mystery. To leverage the limited data available, it is important to understand all the processes that could have shaped our young planet.
S. J. Lock
wiley +1 more source
(Table 2) Selected analyses for garnet pyroxenite and amphibolite samples from the Shackleton Range
Garnet pyroxenite samples = W216, W218, W240, W242A and garnet amphibolite samples = W232, W251 ...
Esther Schmädicke (6973586) +5 more
core +1 more source
Is the garnet amphibolite in the Longyou a retrograded eclogite? [PDF]
A paper titled as “Retrograde garnet amphibolite from eclogite of the Zhejiang Longyou area: New evidence of the Caledonian orogenic event in the Cathaysia block” was recently published in Chinese Science Bulletin (Chen et al., 2015). However, the petrographic features and mineral compositions that authors provided cannot demonstrate that high ...
LiangShu SHU, JinHai YU
openaire +1 more source
A Geophysical Crustal Model of Central Italy for Geoneutrino Predictions in Borexino
Abstract Predicting the geoneutrino signal at underground detectors requires a local crustal reference whose precision matches the experimental uncertainty. The current Borexino reference is 15 years old and deterministic. We replace it with GUESS, a probabilistic 3‐D model of the Gran Sasso region, built by Bayesian inversion of multi‐source ...
L. Rossi +21 more
wiley +1 more source
Azizabad-Hazarkhani granitoid, NE of Songhor: Evidence of a subduction event in the N- Sanandaj-Sirjan continental arc [PDF]
The study area is located in the SaSZ, NE of Songhor city, Kermanshah Province. Based on field observations and mineralogical data, the Azizabad-Hazarkhani I-type calc-alkaline granitoid consists of granites, monzonites and diorites with small volumes of
Ashraf Torkian, , Mohsen Mohammadi
doaj

