《地学前缘》期刊“印度-欧亚大陆碰撞及其远程效应”专题汇集了关于青藏高原及邻区的岩石圈结构、地质构造和地球动力学过程的重要研究论文，这些文章探讨了印度大陆与欧亚大陆碰撞以及青藏高原隆升对地球动力学机制形成与演化的影响。
本专题涵盖了青藏高原的深部探测与岩石圈结构研究，揭示了高原地壳和上地幔的结构，深入探讨了高原隆升的机制。研究主要关注青藏高原的地质构造及演化，深入探讨了不同地区或构造带的地壳深部结构和动力学过程；揭示了印度大陆北漂动力机制，以及大陆碰撞与高原隆升对贝加尔地区的影响。不仅如此，该专辑还包含了在青藏高原开展的技术创新工作，如分布式光纤声传感浅层探测等，为未来深入理解青藏高原的地球动力学过程提供了新的研究思路。
总体而言，该专题既突出了对青藏高原及邻区地质演化和构造过程的深入探讨，为资源环境和地质演化提供了重要理论基础。专题的出版将促进青藏高原多学科的发展与合作，为全球地球科学发展提供新见解。
The special issue of "India-Eurasia Continental Collision and Its Remote Effects" in the Earth Science Frontiers gathers important papers on the lithospheric structure, geological structure, and geodynamic processes of the Tibetan Plateau and its surrounding areas. These articles explore the impacts of the collision between the Indian and Eurasian continents and the uplift of the Tibetan Plateau on the formation and evolution of the Earth's geodynamic system.
This special issue covers in-depth research on the deep exploration and lithospheric structure of the Tibetan Plateau, revealing the structure of the crust and upper mantle, and delving into the mechanisms of plateau uplift. The studies primarily focus on the geological structure and evolution of the Tibetan Plateau, providing profound insights into the deep crustal structures and geodynamic processes in different regions or tectonic zones. Furthermore, the research highlights the driving mechanism for the northward drift of the Indian Plate and the effects of continental collision and plateau uplift on the Baikal region. Additionally, the special issue includes technical innovations conducted in the Tibetan Plateau, such as distributed acoustic sensing for shallow exploration, presenting new research approaches for a deeper understanding of the geodynamic processes in the Tibetan Plateau.
Overall, this special issue emphasizes the geological evolution and tectonic processes of the Tibetan Plateau, providing essential theoretical foundations for environmental resources and geological evolution studies. Its publication will promote interdisciplinary development and collaboration in Tibetan Plateau research and offer new insights for the advancement of global geoscience.
