{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,13]],"date-time":"2025-10-13T15:41:47Z","timestamp":1760370107773,"version":"3.40.4"},"reference-count":103,"publisher":"Geological Society of America","issue":"5-6","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[2025,5,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n               <jats:p>Hybrid zones commonly occur at the contact between different magmatic facies of the same batholith and\/or in contact with the host rock. Fine-grained textures recorded in hybrid zones respond to quenching processes. The compositions of these fine-grained rocks are intermediate and are very close to the silica gap, typically found in calc-alkaline systems. Here, we use examples from the Axial Pyrenean Zone to distinguish types of hybrid zones and examine the potential interest in studying them.<\/jats:p>\n               <jats:p>This study presents new whole-rock geochemistry, mineral chemistry, Rb-Sr and Sm-Nd isotopic data (whole-rock), and geochronological data from magmatic rocks of two plutonic complexes of the Axial Pyrenean Zone (NE Spain). Pennsylvanian calc-alkaline coarse-to fine-grained mafic-intermediate plutonic rocks, including sanukitoid series, intruded the Axial Pyrenean Zone host rocks at ca. 305.8 \u00b1 1.6 Ma (Lys-Caillaouas gabbro), 304 \u00b1 1.7 Ma, and 301.6 \u00b1 1.2 Ma (La Maladeta diorite and granodiorite, respectively). Also, we reviewed the geochemical data of calc-alkaline magmatic rocks from the Pyrenees to compare them with magmas from the sanukitoid and Andean series, which allowed us to consider that they represent a mix between the two series. Petrographic and geochemical results also support that parental magmas were quenched at these hybrid zones. Near-liquidus experiments testing the parental magma composition recorded in hybrid zones shed light on the ultra-high temperatures exceeding 1000 \u00b0C for these magmas to arrive at crustal levels at near-liquidus conditions and account for the need for mantle input to generate these calc-alkaline magmas.<\/jats:p>","DOI":"10.1130\/b37789.1","type":"journal-article","created":{"date-parts":[[2025,2,3]],"date-time":"2025-02-03T21:06:01Z","timestamp":1738616761000},"page":"2784-2802","source":"Crossref","is-referenced-by-count":2,"title":["Ultra-high temperatures recorded in parental magmas from hybrid zones"],"prefix":"10.1130","volume":"137","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-4785-6714","authenticated-orcid":false,"given":"Carmen","family":"Rodr\u00edguez","sequence":"first","affiliation":[{"name":"1Instituto Andaluz de Ciencias de la Tierra (IACT), Consejo Superior de Investigaciones Cient\u00edficas (CSIC)\u2013Universidad de Granada, 18100 Armilla, Granada, Spain"}]},{"given":"Manuel Francisco","family":"Pereira","sequence":"additional","affiliation":[{"name":"2Departamento de Geoci\u00eancias, Center for Sci-Tech Researching Earth System and Energy (CREATE), Escola de Ci\u00eancias e Tecnologia (ECT), Universidade de \u00c9vora, Apt. 94, 7002-554 \u00c9vora, Portugal"}]},{"given":"Joan","family":"Mart\u00ed","sequence":"additional","affiliation":[{"name":"3Department of Geosciences, Institute of Environmental Assessment and Water Research (IDAEA)-CSIC, c\/Jordi Girona St., 18-26, 8034 Barcelona, Spain"}]},{"given":"N\u00faria","family":"Bach","sequence":"additional","affiliation":[{"name":"4Geosciences Barcelona, Applied Volcanology Team, GEO3BCN (CSIC), c\/Llu\u00eds Sol\u00e9 i Sabar\u00eds s\/n, 08028, Barcelona, Spain"}]},{"given":"Noah","family":"Scahmuells","sequence":"additional","affiliation":[{"name":"4Geosciences Barcelona, Applied Volcanology Team, GEO3BCN (CSIC), c\/Llu\u00eds Sol\u00e9 i Sabar\u00eds s\/n, 08028, Barcelona, Spain"}]}],"member":"257","published-online":{"date-parts":[[2025,2,3]]},"reference":[{"key":"2025050211031860200_B1","doi-asserted-by":"crossref","first-page":"55","DOI":"10.1086\/628834","article-title":"Segregation vesicles, gas filter-pressing, and igneous differentiation","volume":"92","author":"Anderson","year":"1984","journal-title":"The Journal of Geology"},{"key":"2025050211031860200_B2","doi-asserted-by":"crossref","first-page":"765","DOI":"10.1093\/petrology\/egv016","article-title":"Differentiation conditions of a basaltic magma from Santorini, and its bearing on the production of andesite in arc settings","volume":"56","author":"And\u00fajar","year":"2015","journal-title":"Journal of Petrology"},{"key":"2025050211031860200_B3","first-page":"167","article-title":"Composici\u00f3n e implicaciones barom\u00e9tricas de los anf\u00edboles en el Complejo Plut\u00f3nico de la Maladeta (Pirineos Centrales, Huesca-L\u00e9rida). 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