Advances in Mantle–Crust Interactions for Petrogenesis and Ore-Forming Processes

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

Deadline for manuscript submissions: 31 December 2024 | Viewed by 151

Special Issue Editors


E-Mail Website
Guest Editor
State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
Interests: isotope geochemistry; igneous petrology; mineralogy chemistry; geochronology; Tethyan evolution

E-Mail Website
Guest Editor
State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
Interests: composition of continental crust; arc magmatism; igneous rocks; Tethyan evolution

E-Mail Website
Guest Editor
Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
Interests: magmatic processes; magma dynamics

E-Mail Website
Guest Editor
Hebei Key Laboratory of Strategic Critical Mineral Resources, College of Earth Sciences, Hebei GEO University, Shijiazhuang 050031, China
Interests: isotope geochemistry; igneous petrology; geochronology; central Asian Orogenic Belt evolution; supercontinent evolution
Special Issues, Collections and Topics in MDPI journals

E-Mail
Guest Editor
Department of Earth System Sciences, Yonsei University, Seoul 03722, Republic of Korea
Interests: petrology; geochemistry; tectonics; magmatism; metamorphism; metasomatism; fluids; pseudosection modeling

Special Issue Information

Dear Colleagues,

Mantle–crust interactions are the central focus of petrological research. Enhanced rock sampling and analytical advancements empower geologists to discern the intricate material exchange processes within the deep lithosphere. Whether through the disruption of ancient cratons or the upwelling of mantle-derived materials during continental collision orogenic events, these interactions profoundly reshape the lithospheric structure and composition. For example, the replacement of ancient lithospheric material with juvenile counterparts and the continuous growth and thickening of the crust occur. In addition, mantle–crust interactions provide vital ore-forming materials and requisite physical-chemical conditions, such as temperature, pressure, and oxygen fugacity, crucial for mineralization. Recognizing these interactions is pivotal for understanding petrogenesis and mineralization, contributing significantly to advances in petrology and ore-forming processes. This Special Issue aims to address, but is not limited to, the following topics:

  1. Developing geochemical indicators for identifying mantle–crust interactions in magmatic processes.
  2. Investigating variations in the strength of mantle–crust interactions during lithospheric evolution and their geodynamic processes.
  3. Determining the origin of ore-forming materials in specific magmatic deposits—whether from the mantle, crust, or a combination of both.
  4. Identifying the magmatic evolution processes (e.g., magma mixing, assimilation, and fractional crystallization) during magma ascent and emplacement and their impacts on petrogenesis and mineralization.

Dr. Feng Huang
Dr. Liang Guo
Dr. Xiyao Li
Dr. Zhiwei Wang
Dr. Vinod Samuel
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

  • mantle–crust interactions
  • petrology
  • geochemistry
  • magmatic evolution
  • mineralization

Published Papers

This special issue is now open for submission, see below for planned papers.

Planned Papers

The below list represents only planned manuscripts. Some of these manuscripts have not been received by the Editorial Office yet. Papers submitted to MDPI journals are subject to peer-review.

1. Zhi-Xin Han et. al Metallogenic significance of monzonite porphyry and magmatic tectonism in Zhangjiawa skarn-type iron deposit, western Shandong, North China Craton

2. Hao-Yuan Lan et. alGeochronology and geochemistry of granites in the Qianliyan Island: response to collision and assembly of the South and North China blocks

3. Li-Jie Jin et. al Petrogenesis of the Early Cretaceous diorite porphyrite in the Xintai region of southwest Shandong, North China Craton: constrains from geochemistry, mineralogy and Sr-Nd-Hf isotopes

4. Ling Chen et. al Petrogenesis and tectonic implications of the early Paleozoic plutons in the Sheshan of the Dayaoshan Uplift, south China

5. Shashank Prabha-Mohan, Ian S. Williams, Sandeep Singh. Zircon, Monazite SHRIMP U-Th-Pb and Quartz Oxygen Isotopic Results from the Higher Himalayan Crystallines (HHC) of the Sikkim Himalayas, India

 

Back to TopTop