2-2-2-2-2-2-2-2-2-2-2-2-2 From: Pablo Jorge Caffe <pabcaffe@xxxxxxxxxxxxxxxxx> Dear colleagues We want to draw your attention about the deadline extension for the final reception of manuscripts that will be included in the Special Issue of Journal of South American Earth Sciences "Phanerozoic magmatism of the Central Andes. Petrology, volcanism, geotectonic setting and metallogenic meaning: a tribute to Beatriz Coiraâ??s scientific legacy". The new deadline has been set by October 31 2025. We are grateful for all the contributions proposed until now, and want to let you know that the Guest Editorial Board is still open to receive contribution proposals from those authors that find their work suitable for the scope of this VSI. https://www.sciencedirect.com/special-issue/318710/phanerozoic-magmatism-of-the-central-andes-petrology-volcanism-geotectonic-setting-and-metallogenic-meaning-a-tribute-to-beatriz-coira-s-scientific-legacy <https://urldefense.com/v3/__https://www.sciencedirect.com/special-issue/318710/phanerozoic-magmatism-of-the-central-andes-petrology-volcanism-geotectonic-setting-and-metallogenic-meaning-a-tribute-to-beatriz-coira-s-scientific-legacy__;!!IKRxdwAv5BmarQ!aVnoV91mn5_PDDk5p8LPHeh9UuN2CiPTq2l1C8zIbVSyrpXF2SW5mBA6d3_jiR3Zv0a-02-DhDK315X787k3-yVL_w$> All the best, Dr Pablo J. Caffe Guest Editor JSAES Special Volume - Journal of South American Earth Sciences Phanerozoic magmatism of the Central Andes. Petrology, volcanism, geotectonic setting and metallogenic meaning: a tribute to Beatriz Coiraâ??s scientific legacy. Deadline for reception of manuscripts October 31, 2025. The work of Dr. Beatriz Coira (Betty) has been a point of reference for the study of Cenozoic and pre-Cenozoic volcanism of the central Andean region. Her career, which started in 1964 with a Mineralogy Assistant position in the Dirección Nacional de GeologÃa y MinerÃa, and followed up as a CONICET Researcher, Full Professor of Petrology, and Head of the Instituto de GeologÃa y MinerÃa (Jujuy National University), has been devoted to the study of different aspects of magmatism: geological mapping, volcanic stratigraphy, petrography, petrology and geochemistry of various types of igneous rocks, as well as hydrothermal alteration and ore deposit genesis in northwestern Argentina, especially in the Puna, and regions nearby. She was able to reconstruct the complex petrogenesis of these magmatic systems, the modeling of eruption mechanics and the broad geodynamic context in which they occurred. Additionally, she explored the role of magmatism in the location and genesis of current and fossil hydrothermal systems as well as in ore deposit formation. During her prolific career, which still continues, Dr. Coira published hundreds of peer-reviewed papers in prestigious national and international journals, as well as contributions in proceedings, reports, bulletins, and geological charts. She taught courses at the graduate and postgraduate levels and supervised dozens of students with constant dedication and sense of excellency. She was many times awarded for her remarkable work and scientific merit by renowned academic and scientific organizations of Argentina and the world. In this Special Issue of JSAES, we want to honor the scientific legacy and pioneer career of Betty Coira with a collection of new contributions dealing with the central Andean Phanerozoic magmatism. We invite the Earth Sciences community to contribute manuscripts dealing with issues such as field geology, geochemistry, petrology, mineralogy, ore deposit and hydrothermal alteration studies, as well as structural geology and geophysics linked to the magmatism developed in the central Andean region from Cambrian to Recent time. Guest Editors: - Pablo J. Caffe, INECOA-UNJu. Argentina. pabcaffe@xxxxxxxxxxxxxxxxx - Jorge Clavero Ribes. Amawta Geoconsultores, Chile. jclavero@xxxxxxxxx - Clara E. Cisterna. UNT. Argentina. claracisterna@xxxxxxxxxxxxxxxx - Guadalupe Maro. INECOA-UNJu. Argentina. g.maro@xxxxxxxxxxxxxx - Michael Ort. Trinity College Dublin. Irlanda. mtablescrap@xxxxxxxxx 2-2-2-2-2-2-2-2-2-2-2-2-2 ------------------------------
