• 责任者：Li Zhong (Institute of Geology and Geophysics ; Chinese Academy of Sciences ; Beijing 100029 ; China) ; Xu Jianqiang
• 刊名：Acta Sedimentologica Sinica
• 出版年：2013
• 卷期：31(5)
• 关键词：盆山耦合 ; basin range coupling ; 沉积学 ; sedimentology ; 华北地区 ; North China ; 塔里木盆地 ; Tarim Basin
• 页码：p.757-772
• 图表：5 illus., 1 table, 142 refs.
• 分类号：0803
• issnNo：ISSN1000-0550
• isbnNo：CN62-1038/P

     Basin-range system, as a new geological unit or entity, has been accepted and studied in geosciences. Based on reviews on the past research advances, three rules are brought forward for basin-range classification, which includes plate tectonic unit （location）, tectonic geodynamical regime, and paleogeographical or tectonic-sedimentary attributes of source-sink systems. There  are  three basin-range types, intracontinent, continent margin （continent-ocean） and intraocean, and further fourteen sub-typies can be presented in the classification scheme. Then a research frame of basin-range system sedimentology is stated and discussed, in which the tectonic-stratigraphic unit and isochronal stratigraphic framework, provenance tracing and source-sink system, and integrated depositional records and paleotectonic-paleoclimatic evolution are three important research basises; and the depositional system （tract） and integrated tectonic-paleogeography is research core; and the basin-range evolution geodynamics is an subject target of basin-range system sedimentology. As a case study of intracontinent basin-range system in eastern North China, the research shows that the most prominent basin-range system occurred in north North China during Jurassic-early Early Cretaceous due to collision and uplift process between Siberia block and North China-Mongolia one. However, a coexistent source-sink system related to the Su-Lu orogen has weak influences on sedimentary paleogeography of the North China. As another case study of continent margin basin-range system in Tarim area, northwest China, the research basicially reveals differential geological records, reflecting passive and arc-related continent margin basin-range systems, respectively coexisted between west South Tianshan and east one. Finally, in order to deepen the basin-range geodynamics, it is especially suggested to pay attention to academic researches of the provenance tracing and source-sink system and the integrated depositional records and paleotectonic-paleoclimatic evolution.