了解库柏盆地的盆地构造、沉积环境和沉积路径之间的相互作用

C. Wainman, P. McCabe
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摘要

晚石炭世至中三叠世的库珀盆地是澳大利亚主要的陆上石油省,拥有一系列常规和非常规资源(Hall et al., 2019)。尽管Cooper盆地被认为是一个成熟的含油气盆地,已经钻探了1900多口井,进行了104,000多公里的地震勘探(Resources, 2022),但由于8个海槽和中间山脊之间的构造和沉积历史非常不同,Cooper盆地的许多方面仍然是一个谜(Kulikowski等人,2022)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Understanding the interplay between basin architecture, depositional environments and sediment pathways in the Cooper Basin
The late Carboniferous to Middle Triassic Cooper Basin is Australia’s premier onshore petroleum province hosting a range of conventional and unconventional resources (Hall et al., 2019). Despite being considered a mature petroleum basin with over 1900 wells drilled and over 104,000 km of seismic surveys shot (Resources, 2022), many aspects of the Cooper Basin remain enigmatic with very different structural and sedimentary histories between the eight troughs and intervening ridges (Kulikowski et al., 2022).
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