国内外学者对华北克拉通金矿床开展了大量深入研究，积累了丰富资料，取得了系列重要进展。但对已有成果的总结、对比和融合还不够，对华北克拉通破坏与金矿床的成因联系仍缺乏多学科的综合分析与集成，区域与全球对比研究亟需加强。本项目围绕《华北克拉通破坏》重大研究计划的总体目标，全面总结和集成克拉通破坏与成矿作用研究的系列成果，深入分析华北克拉通金矿床成因机制尚未解决的关键问题和争论的焦点，针对“华北克拉通破坏与矿产资源聚集的关系”这一核心科学问题进一步开展多学科交叉研究，揭示华北克拉通破坏深部过程尤其是深部岩浆活动与成矿的关系，进一步提升对大洋板块俯冲、克拉通岩石圈破坏、壳幔岩浆活动与金成矿作用成因联系的理论认识。开展全球对比，深化对克拉通破坏成矿效应的理解。基于上述成果集成，开展小秦岭矿集区金矿床深部成矿规律、关键控矿因素、矿体定位规律的多学科联合攻关，科学评价深部成矿潜力和预测找矿有利空间。

Significant advance has been made in our understanding of late Mesozoic gold mineralization over the North China craton after extensive studies by domestic and overseas researchers. In the past decade, massive data and numerous papers have been accumulated, but little has been done in data integration, leaving metallogenic information of various data largely unexplored. In addition, comparative studies have been rarely conducted for gold deposits from distinct districts and, particulalrly, there is a lack of multi-disciplinary studies aiming to provide tight constraints on the genetic link between the craton-wide gold metallogeny and decratonization processes. Lastly, how the extent, styles, and evolution of gold mineralization has responded to the destruction of modification of the world's cratons remains poorly understood due to a lack of global perspective. The proposed research aims at the overall objectives of the big research plan of “Decratonization of the North China Craton” and make a comprehensive review and summary of the research finding on decrationization and its related gold deposits. Focusing on the key scientific question “genetic link between decrationization and metallogeny”, we will use multidisciplinary methods to figure out the deep processes of decratonization, particularly the connection between magmatism in the deep crust and formation of mineral deposits. The project would yield results that advance our understanding in the possible links of subduction of oceanic crust, decrationization, mantle-derived magmatism and gold mineralization. In order to further understand decratonization and its effect on ore formation, a comparative study will be carried out between gold mineralization in North China craton and other Precambrian cratonic blocks elsewhere that have partly lost their lithospheric roots . On the basis of data integration and regional and global comparative studies, we will plan to carry out a multi-disciplinary study on metallogenesis, key ore-controlling factors, localization of deep-seated orebodies in the Xiaoqinling district. We then finally make a scientific evaluation on the mineralization potential of deep part of known deposits and prediction of favorable sites for ore prospecting.