From Cycles to Sequences:Sequence Stratigraphy and Relative Sea Level Change for the Late Cambrian of the North China Platform |
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| Authors: | MEI Mingxiang MA Yongsheng DENG Jun and CHEN Huijun Key Laboratory of Lithospheric Tectonics and Lithoprobing Technology of the Education Ministry China University of Geosciences Beijing |
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| Institution: | MEI Mingxiang,MA Yongsheng,DENG Jun and CHEN Huijun Key Laboratory of Lithospheric Tectonics and Lithoprobing Technology of the Education Ministry,China University of Geosciences,Beijing,Department of Oil-Fields,China Petrochemical Corporation,Beijing |
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| Abstract: | Abstract In the Late Cambrian, the North China Platform was a typical carbonate ramp platform. The Upper Cambrian of the northern part of the North China Platform is famous for the development of bioherm limestones and storm calcirudites and can be divided from bottom to top into the Gushan, Changshan and Fengshan formations. In this set of strata, the deep‐ramp mudstone and marls and the shallow‐ramp packstones and grainstones constitute many carbonate meter‐scale cycles of subtidal type. More tidal‐flat dolomites are developed in the Upper Cambrian of the southern margin of the North China platform, in which limestone and dolomite beds also constitute many carbonate meter‐scale cycles of the peritidal type. These cycles are marked by a variety of litho‐facies successions. There are regularly vertical stacking patterns of meter‐scale cycles in long‐term third‐order sequences, which is the key to discerning such sequences. Third‐order sequence is marked by a particular sedimentary‐facies succession that is the result of the environment‐changing process of deepening and shoaling, which is genetically related to third‐order sea level changes. Furthermore, four third‐order sequences can be grouped in the Upper Cambrian of the North China Platform. The main features of these four third‐order sequences in the northern part of the platform can be summarized as follows: firstly, sequence‐boundaries are characterized by drowning unconformities; secondly, the sedimentary‐facies succession is generally constituted by one from deep‐ramp facies to shallow‐ramp facies; thirdly, a succession of “CS (?)+HST” (i.e., “condensed section and high‐stand system”) forms these four third‐order sequences. The chief features for the third‐order sequences in the southern part of the North China Platform comprises: more dolomites are developed in the HSTs of third‐order sequences and also developed more carbonate meter‐scale cycles of peritidal types; the sedimentary‐facies succession of the third‐order sequences is marked by “shallow ramp‐tidal flat”; the sequence boundaries are characterized by exposure punctuated surfaces. According to the changes for the third‐order sequences from the north to the south, a regular sequence‐strati graphic framework can be established. From cycles to sequences, the study of sequence stratigraphy from litho‐facies successions to sedimentary‐facies successions exposes that as follows: meter‐scale cycles that are used as the basic working unit actually are litho‐facies successions formed by the mechanism of a punctuated aggradational cycle, and third‐order sequences that are constituted by regularly vertical stacking patterns of meter‐scale cycles are marked by sedimentary‐facies successions. On the basis of the changing curve of water depth at each section, the curve of the relative third‐order sea level changes in the late Cambrian of the North China Platform can be integrated qualitatively from changing curve of water depth. The correlation of Late Cambrian long‐term sea level changes between North China and North America demonstrates that there are not only similarities but also differences, reflecting control of long‐term sea level changes both by global eustacy and by regional factors. |
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| Keywords: | squence stratigraphy relative sea level changes Late Cambrian North China Platform |
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