摘要:
根据层序关键界面、体系域叠置关系及内部构型特征,结合生物地层资料,右江盆地泥盆系可划分为17个三级层序,其中下统 7个、中统 5个、上统 5个,包括 9个Ⅰ型层序、8个Ⅱ型层序,代表17次三级相对海平面变化产物。在此基础上,对不同沉积背景的层序进行了对比,建立了相应的层序格架模型。结果表明,不同沉积相带的层序内部构型和成因格架存在一定的差异,但由于海平面变化这一共同因素的影响,它们仍可进行对比和追踪。
Abstract:
Based on key sequence boundary, sedimentary system tracts, in conjunc tion with bio-stratigraphy, sequence stratigraphy during the Devonian in the Yo ujiang Basin has been studied in detail. 17 3rd-order sequences have been recog nized for the first time, 7 sequences in the Lower, 5 sequences in the Middle an d 5 sequences in the Upper Devonian, including 10 Ⅰ-type sequences and 7 Ⅱ-t ype sequences, representing 17 3rd-order relative sea level changes. Moreover, sequences in different sedimentary backgruonds have been correlated and then cor responding seqence stratigaphic framework has also been established. This paper demonstrated that sequence internal architecture and genetic framework within va rious sedimentary facies zones are obviously different, but they can be correlat ed and traced because of the same control factor-relative sea level changes. The Devonian transgression in this area extended from south to north overlappe d in the formation of the transgression-type sequences. These sequences were co ntrolled by sea-level change and tectonic activities. At least three 2nd-order rising sea level stages have been distinguished. During the basin evolution, the late stage of Early and Middle Devonian and the early of Late Devonian correspo nd to the eustatic change of sea level. During these periods the tectonic, volca nism and sedimentary differentiation might be very strong. Devonian basin can be subdivided into stability and riftplatform. the former distributes in Lochkovian, Pragian, Eifelian, Frasnian and Famenian, and the latter in Emrian and Givetian. In the stability age, sequences can be correlated one by one. But in tectonic area period, sequences are clearly different. The r esult of research shows that Devonian sequence of stabilized platform area is ma inly controlled by sea ieel change and tectonic movement of the globe or the r egion, and the sequence of the rift trough in the platform is controlled by the basement tectonics of the basin and the episodic subsidence.
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