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首页> 外文期刊>Geo-marine letters >Seismic expression and inferred depositional environments of Plio-Pleistocene sedimentary sequences in the southwestern Caspian Sea
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Seismic expression and inferred depositional environments of Plio-Pleistocene sedimentary sequences in the southwestern Caspian Sea

机译:里海西南部上新世-新世沉积序列的地震表达和推断沉积环境

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摘要

Eight seismic profiles from the southwestern Caspian Sea were analyzed to establish the sedimentary environments and depositional history in the South Caspian Basin since Pliocene times. Based on reflection terminations, nine sequence boundaries (S1 to S9) were identified and traced across the study area. Consequently, nine depositional sequences (S1-S9) were defined on the basis of seismic facies analysis. The results suggest a transition from non-marine sedimentation in the Lower Pliocene to marine-dominated conditions in the Upper Pliocene (S1-S4). Marine conditions then continued to the present time; however, several sea-level changes led to the formation of sequences S5 to S9. Although no local sea-level curve is available due to a lack of well data, there is good agreement between the seismic stratigraphy of the study area and a published regional sea-level curve.
机译:分析了上新世以来西南里海的八个地震剖面,以建立南里海盆地的沉积环境和沉积历史。基于反射终止,确定了九个序列边界(S1至S9)并在研究区域内进行了追踪。因此,根据地震相分析确定了9个沉积层序(S1-S9)。结果表明从上新世下层的非海洋沉积向上新世上层(S1-S4)的海洋为主的条件转变。然后,海洋状况一直持续到现在。但是,几次海平面变化导致形成了序列S5至S9。尽管由于缺乏井眼数据而无法获得局部海平面曲线,但研究区域的地震地层学与已发布的区域海平面曲线之间存在着很好的一致性。

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