[HTML][HTML] The Mid-Variscan Allochthon: Keys from correlation, partial retrodeformation and plate-tectonic reconstruction to unlock the geometry of a non-cylindrical belt

JRM Catalan, K Schulmann, JF Ghienne - Earth-Science Reviews, 2021 - Elsevier
The non-cylindrical character of the Variscan Belt is established via a description of its most
salient geological characteristics and correlations among the main and relatively minor …

Conditions during the formation of granitic magmas by crustal melting–hot or cold; drenched, damp or dry?

JD Clemens, G Stevens, SE Bryan - Earth-Science Reviews, 2020 - Elsevier
Granitic magmas extracted from crustal sources can form over a wide variety of P, T and aH
2 O conditions. Both fluid-present and effectively fluid-absent conditions can yield granitic …

[HTML][HTML] What can we learn from melt inclusions in migmatites and granulites?

B Cesare, A Acosta-Vigil, O Bartoli, S Ferrero - Lithos, 2015 - Elsevier
With less than two decades of activity, research on melt inclusions (MI) in crystals from rocks
that have undergone crustal anatexis–migmatites and granulites–is a recent addition to …

Granitoid magmas preserved as melt inclusions in high-grade metamorphic rocks

O Bartoli, A Acosta-Vigil, S Ferrero… - American Mineralogist, 2016 - degruyter.com
This review presents a compositional database of primary anatectic granitoid magmas,
entirely based on melt inclusions (MI) in high-grade metamorphic rocks. Although MI are …

Micropetrology: Are inclusions grains of truth?

S Ferrero, RJ Angel - Journal of Petrology, 2018 - academic.oup.com
Inclusions in minerals, whether fluids, melts or crystalline phases, are small pieces of the
large-scale puzzle of Nature, time-consuming to investigate and often of difficult …

[HTML][HTML] C–O–H fluid-melt-rock interaction in graphitic granulites and problems of quantifying carbon budget in the lower continental crust

BB Carvalho, O Bartoli, B Cesare - Chemical Geology, 2023 - Elsevier
Estimates on the geological carbon cycle are subject to large uncertainties that can be
reduced by thorough observation of rocks. In this contribution, we focus specifically on C–O …

Lithological successions of the internal zones and flysch trough units of the betic chain

A Jabaloy Sánchez, A Martín-Algarra… - The Geology of Iberia: A …, 2019 - Springer
Mesozoic lithological successions of the Alborán domain record two rifting events. An initial
Triassic rifting stage is characterized by thick stratigraphic successions showing typical …

Lateral variations of pressure-temperature evolution in non-cylindrical orogens and 3-D subduction dynamics: the Betic-Rif Cordillera example

E Bessière, L Jolivet, R Augier… - Bulletin de la …, 2021 - pubs.geoscienceworld.org
Abstract The long-term Pressure-Temperature-time-deformation (PTtd) evolution of the
internal zones of orogens results from complex interactions between the subducting …

Pre-Alpine prograde evolution of the Upper Alpujarride (Betic-Rif belt) reveals a Paleotethys-related collision

A Sánchez-Navas, A Martín-Algarra… - International Geology …, 2024 - Taylor & Francis
Medium and high grade kyanite-bearing graphitic metapelites of the basement of the Torrox
Unit (Upper Alpujarride, Western Mediterranean) show kyanite-andalusite-kyanite …

Hercynian anatexis in the envelope of the Beni Bousera peridotites (Alboran Domain, Morocco): Implications for the tectono-metamorphic evolution of the deep crustal …

F Rossetti, F Lucci, T Theye, M Bouybaouenne… - Gondwana …, 2020 - Elsevier
The metamorphic core of the Betic-Rif orogenic chain (Alboran Domain) is made up of lower
crustal rocks forming the envelope of the Ronda (Spain) and Beni Bousera (Morocco) …