• 责任者：Kong Fanmei (Key Laboratory of Depositional Mineralization & Sedimentary Minerals ; Institute of Geological Science and Engineering ; Shandong University of Science and Technology ; Qingdao 266510 ; China) ; Li Xuping
• 刊名：Geological Review
• 出版年：2011
• 卷期：57(5)
• 关键词：杂岩 ; complexes ; 黑龙江省 ; Heilongjiang Province
• 页码：p.623-631
• 图表：5 illus., 52 refs.
• 分类号：0802
• 出版序号：1670
• issnNo：ISSN0371-5736
• isbnNo：CN11-1952/P

The Heilongjiang complex zone like a belt from south to north exposed to the east of Jiayin-Mudanjiang suture zone. Studies indicate that the Heilongjiang complex zone is mainly formed from the late Hercynian to Indosinian. Geochemical characteristics suggest a geological background of the oceanic crust subduction and collision of the Jiamusi Massif and the Songnen Block (Songhua River-Nenjiang River Block). Combined with isotope study, paleontological research and geological background of the Jiamusi Massif, this study sums up a formation and evolution model of the Heilongjiang complex, and develops a lithofacies paleogeography diagram of Late Carboniferous to Early Permian in Northeast China.