1. Analyses of the Sea Level Curve Based on High-precision Carbonate Microfacies.
- Author
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MU CaiNeng, HOU MingCai, LIU XinChun, ZHANG HongRui, and FAN ChengHua
- Abstract
The variation of an accurate global sea level curve has always been a difficult and frontier scientific problem in sedimentary geological research. There are 2 reasons: (1) the deep-time sedimentary record is the comprehensive response to global sea level change and regional movement, but accurately eliminating the regional tectonic effect is also difficult; (2) determining paleo-water depth based on deep-time sedimentary records is still being explored. The Kalpin area of the Tarim Basin in the Late Ordovician experienced an environmental evolution from basin to basin margin to shelf, making it highly sensitive to sea level changes and an ideal area for conducting research on sea level changes based on sedimentary microfacies. The study conducted a detailed field investigation and intensive sampling analysis of the Dawangou section. Based on lithofacies sedimentology, paleontology, etc., the two major fa-cies of the continental shelf and the basin edge were divided, and seven microfacies are distinguished in detail: MF1, brick red/purple microbial micritic limestone; MF2, gray microbial micritic limestone; MF3, gray-green calcareous clay; MF4, gray bioclastic - lithoclastic breccia limestone; MF5, gray bioclastic silty limestone; MF6, gray bioclastic micritic limestone; and MF7, dark gray calcareous clay. Based on advanced microfacies for the sensitive zone of deep-time sedimentary records, the sea level change curve of the Upper Ordovician Kanling and Yingan Formations is constructed, and a set of methods for determining the global sea level curve can be summarized. Our sea level curve is compared with the upper Yangtze region, the southern margin of Ordos, North America, South America, Wales, and the global sea level change, and results indicate that the frequent fluctuations of sea level are similar to North America. The reconstruction plate tectonic results of the study indicate that the Caledonian tectonic movement has global corresponding characteristics during this period. Frequent plane fluctuations are mainly caused by orogenic collisions in different regions. [ABSTRACT FROM AUTHOR]
- Published
- 2021
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