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ORIGINAL RESEARCH article
Front. Phys.
Sec. Social Physics
Volume 13 - 2025 | doi: 10.3389/fphy.2025.1557932
This article is part of the Research Topic Finance and Production Complex Systems View all 5 articles
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With the development of global industrialization, metal minerals have become a global focal point of great power competition. An in-depth investigation into the evolution of global mineral trade structures, alongside an analysis of the relationships between metal minerals trade, resource endowments, industrialization, regional dynamics, and geopolitical competition, is crucial for nations to formulate effective trade policies and enhance the stability of global mineral trade development. This study explores the evolution trends of the global metal minerals trade structure from 1990 to 2022 based on complex network and further detect community structure using the Infomap algorithm. The results show that (1) There is a general upward trend in global metal minerals trade from 1990 to 2022, which can be segmented into phases of slow, rapid, and moderate growth. (2) The two major trading circles formed in the early stage with Japan and Europe as the center have changed, forming a dual pattern with China as the super demand center and Australia as the super supply center. (3) China, Australia, the U.S., Japan, Brazil, and the European Union play key roles in shaping the global trade network, with the structure of the global metal minerals trade network primarily being driven by demand centers. (4) According to the economic trends and the evolving resource demands, the global trade structure will translate from a concentrated bipolar model to a diversified network with multiple trade centers. The conclusion of this research helps specify international policies and maintain supply chain resilience.
Keywords: Metal minerals, international trade, Complex Network, Map equation framework, community detection
Received: 09 Jan 2025; Accepted: 13 Feb 2025.
Copyright: © 2025 Zhang, Chen, Wang, Guan, Xing, Long, Zheng, Li and Shang. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence:
Qishen Chen, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China
Kun Wang, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China
Jiayun Xing, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China
Tao Long, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China
Guodong Zheng, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China
Mei Li, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China
Chenghong Shang, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China
Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.
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