Igneous Rocks as Archives of Earth's Geological History: Magma Processes and Continental Crust Evolution

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Geochemistry and Geochronology".

Deadline for manuscript submissions: 30 November 2025 | Viewed by 708

Special Issue Editors


E-Mail Website
Guest Editor
Department of Earth Sciences, Ibaraki University, 2-1-1, Bunkyo, Mito 310-8512, Japan
Interests: volcanology; volcanic rocks; caldera; pleaomagnetism

E-Mail Website
Guest Editor
Department of Earth and Planetary Sciences, Faculty of Geography, Universitas Gadjah Mada, Yogyakarta, Indonesia
Interests: volcanology; physics of magmatic properties; dynamics of volcanic eruptions; caldera; stratigraphy

E-Mail Website
Guest Editor
Department of Applied Chemistry for Environment, School of Biological and Environmental Sciences, Kwansei Gakuin University, Sanda 669-1330, Japan
Interests: petrology; plutonic rocks; granite

Special Issue Information

Dear Colleagues,

Igneous rocks are archives of the Earth’s history. Both volcanic and plutonic rocks can predict the age of when a mineral crystalized from a magma, i.e., essentially when the rock was formed. The combination of such chronological data with petrographical and petrochemical analyses of igneous rocks thus offers a powerful tool for reconstructing Earth’s evolutionary history and for investigating Earth’s interior processes, such as the crustal magma plumbing systems beneath volcanic fields and the growth of continental crust.

This Special Issue focuses on studies where geochronology (e.g., radiometric dating, paleomagnetic dating) and petrology (e.g., mineral chemistry, crystal size distribution) of volcanic/plutonic rocks are used to evaluate magmatic processes, including both subsurface volcanism and abyssal plutonism in the continental crust. We also welcome fundamental research, such as the incorporation of high-precision dating to constrain petrogenesis and magmatic tempos in specific study areas.

Dr. Takeshi Hasegawa
Dr. Indranova Suhendro
Dr. Kazuya Shimooka
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Minerals is an international peer-reviewed open access monthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2400 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • igneous rock
  • continental crust
  • magma process
  • geochronology
  • volcanism
  • plutonism

Benefits of Publishing in a Special Issue

  • Ease of navigation: Grouping papers by topic helps scholars navigate broad scope journals more efficiently.
  • Greater discoverability: Special Issues support the reach and impact of scientific research. Articles in Special Issues are more discoverable and cited more frequently.
  • Expansion of research network: Special Issues facilitate connections among authors, fostering scientific collaborations.
  • External promotion: Articles in Special Issues are often promoted through the journal's social media, increasing their visibility.
  • Reprint: MDPI Books provides the opportunity to republish successful Special Issues in book format, both online and in print.

Further information on MDPI's Special Issue policies can be found here.

Published Papers (1 paper)

Order results
Result details
Select all
Export citation of selected articles as:

Research

13 pages, 1341 KiB  
Article
Zircon Systematics of the Shionomisaki Volcano–Plutonic Complex (Kii Peninsula, Japan): A Potential Tool for the Study of the Source Region of Silicic Magmas
by Ulrich Knittel, Monika Walia and Shigeyuki Suzuki
Minerals 2025, 15(5), 537; https://doi.org/10.3390/min15050537 - 18 May 2025
Viewed by 273
Abstract
The Shionomisaki Igneous Complex is part of the Mid Miocene igneous province developed within the Shimanto Accretionary Complex in front of the volcanic front in SW Japan. The igneous rocks in this province mostly have silicic compositions. New U-Pb ages obtained for two [...] Read more.
The Shionomisaki Igneous Complex is part of the Mid Miocene igneous province developed within the Shimanto Accretionary Complex in front of the volcanic front in SW Japan. The igneous rocks in this province mostly have silicic compositions. New U-Pb ages obtained for two samples from the Shionomisaki Complex at the southern tip of the Kii Peninsula (14.6 ± 0.4 Ma and 14.9 ± 0.4 Ma) fall into the range of previous age determinations (14.6 ± 0.2 to 15.4 ± 0.3 Ma). Hf isotopic compositions obtained for co-magmatic zircon (εHf(t) = −0.7 to +4.8) lie between typical values obtained for mantle-derived magmas and values obtained for old crustal rocks. They are thus consistent with previous interpretations that the magmas are mixtures of mantle and crustally derived magmas. In the modelling of the isotopic characteristics of the magmas, the sediments of the Shimanto belt are taken as the protolith of the silicic magmas. Xenocrystal zircon (i.e., zircon picked up during ascent and emplacement of the magma) found in the silicic igneous rocks exhibits a similar age pattern as detrital zircon of the Shimanto sediments. However, the age pattern obtained in this study for zircon cores, which are considered to be restitic zircon (i.e., zircon derived from the source of the anatectic melt), shows little semblance with the age pattern of Shimanto sediments. It is, therefore, tentatively suggested that the source area of the silicic magmas may not be identical with the sediments of the Shimanto Accretionary Complex. Full article
Show Figures

Figure 1

Back to TopTop