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高校地质学报 ›› 2020, Vol. 26 ›› Issue (4): 395-410.DOI: 10.16108/j.issn1006-7493.2020020

• 深时数字地球专辑: 地球科学大数据II • 上一篇    下一篇

深时全球海平面变化重建方法的回顾与展望

许艺炜,胡修棉   

  1. 南京大学 地球科学与工程学院,南京 210023
  • 出版日期:2020-08-20 发布日期:2020-08-20

Review and Prospects of Studying Methods to Reconstruct Eustatic Sea-level Changes in Deep-time

XU Yiwei,HU Xiumian   

  1. School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China
  • Online:2020-08-20 Published:2020-08-20

摘要: 全球海平面变化对古地理、古生物、古气候演化以及能源矿产分布具有重要的控制作用。然而,目前学界对深时海平面变化的驱动机制尚不清楚,部分归因于缺乏高精度全球海平面变化的恢复。文章回顾了全球海平面变化研究的起始与发展过程,归纳出五种类型的深时海平面变化重建方法和技术,即地层学、沉积学、洋盆动力学、同位素地球化学方法和大数据技术。并总结了上述研究方法的原理、优势和不足,并以白垩纪全球海平面重建为实例,讨论了当前深时全球海平面重建的难点和争议点,并对未来深时全球海平面变化重建进行了展望。

关键词: 全球海平面变化, 深时, 地层回剥, 层序地层, 洋盆动力学, 大数据

Abstract: Eustatic sea-level changes strongly control the Earth evolution on paleogeography, paleontology and paleoclimate, as well as the distribution of petroleum and coal deposits. The controlling factors of eustatic sea-level changes are, however, still poorly understood partly due to lack of a high-resolution global sea-level curve. This paper reviewed the history of eustasy research, and summarized five types of approaches to reconstruct eustatic sea-level changes in deep-time, including stratigraphic, sedimentological, ocean basin dynamics, geochemical approaches and big data technique. We take the Cretaceous sea-level curve
as an example to describe the difficulties in reconstructing eustatic sea-level changes and the results displayed that promising prospects could be expected in this area.

Key words: eustatic sea-level change, deep time, back-stripping, sequence stratigraphy, ocean basin dynamics, big data

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