On the origin of quartz in the Velkerri Fm: implications for exploration and production in the Beetaloo Sub-basin and the Si cycle in the Mesoproterozoic

Claudio Delle Piane, K. Milliken, V. Crombez, L. Martin, W. Rickard
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Abstract

The Beetaloo Sub-basin is a concealed, composite depocenter and a component of a group of intra-cratonic Paleoproterozoic to Mesoproterozoic sedimentary basins collectively described as the Greater McArthur Basin. The Sub-basin hosts unconventional and conventional petroleum resources, particularly in the uppermost Roper Group where stacked play opportunities include liquids rich shale, dry gas shale and hybrid/ tight gas plays (Côté et al. 2018; Altmann et al., 2020).
Velkerri组石英成因:对Beetaloo次盆地勘探与生产及中元古代硅旋回的启示
Beetaloo次盆地是一个隐伏的复合沉积中心,是克拉通内古元古代至中元古代沉积盆地的组成部分,这些沉积盆地统称为大麦克阿瑟盆地。该子盆地拥有非常规和常规石油资源,特别是在最上层的Roper组,那里的叠合油气藏包括富液页岩、干气页岩和混合/致密气气藏(Côté et al. 2018;Altmann et al., 2020)。
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