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首页> 外文期刊>The APPEA Journal >THE EASTERN OTWAY BASIN WANGERRIP GROUP REVISITED USING AN INTEGRATED SEQUENCE STRATIGRAPHIC METHODOLOGY
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THE EASTERN OTWAY BASIN WANGERRIP GROUP REVISITED USING AN INTEGRATED SEQUENCE STRATIGRAPHIC METHODOLOGY

机译:使用综合层序地层学方法对东部奥特韦盆地盆地旺格里普集团进行重新评估

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摘要

Recent exploration by BHP Petroleum in VIC/ P30 and VIC/P31, within the eastern Otway Basin, has contributed significantly to our understanding of the depositional history of the Paleocene to Eocene siliciclastic Wangerrip Group. The original lithostratigraphic definition of this group was based on outcrop description and subsequently applied to onshore and, more recently, offshore wells significantly basinward of the type sections. This resulted in confusing individual well lithostratigraphies which hampered traditional methods of subsurface correlation. A re-evaluation of the Wangerrip Group stratigraphy is presented based on the integration of outcrop, wireline well log, palynological and reflection seismic data. The Wangerrip Group can be divided into two distinct units based on seismic and well log character. A lower Paleocene succession rests conformably on the underlying Maastrichtian and older Sherbrook Group, and is separated from an overlying Late Paleocene to Eocene succession by a significant regional unconformity. This upper unit displays a highly progradational seismic character and is named here as the Wangerrip Megasequence. Regional seismic and well log correlation diagrams are used to illustrate a subdivision of the Wangerrip Megasequence into eight third-order sequences. This sequence stratigraphic subdivision of the Wangerrip Group is then used to construct a chronostratigraphic chart for the succession within this part of the Otway Basin.
机译:必和必拓石油公司最近在奥特韦盆地东部的VIC / P30和VIC / P31中进行了勘探,这对我们对古新世至始新世硅质碎屑旺格里普群的沉积历史的认识做出了重要贡献。该组的原始岩相地层学定义是基于露头描述,随后应用于陆上井,以及最近的海上井,明显位于类型剖面的下方。这导致了井眼地层学的混乱,从而阻碍了传统的地下相关方法。基于露头,电缆测井,孢粉学和反射地震数据的整合,对Wangerrip组地层进行了重新评估。根据地震和测井特征,Wangerrip组可以分为两个不同的单元。较低的古新世演替地一致地位于潜在的马斯特里赫特和较早的Sherbrook群上,并且由于明显的区域不整合而与上覆的古新世至始新世演替分离。该上部单元显示出高度渐进的地震特征,在这里被称为Wangerrip Megasequence。区域地震和测井相关图用于说明Wangerrip Megasequence细分为八个三阶序列。然后,将Wangerrip组的层序地层细分用于为奥特韦盆地这一部分的演替构造一个年代地层图。

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