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澳大利亚北卡那封盆地晚三叠世混合沉积特征

黄众 胡孝林 杨松岭 张璐

海相油气地质2018,Vol.23Issue(1):21-28,8.
海相油气地质2018,Vol.23Issue(1):21-28,8.DOI:10.3969/j.issn.1672-9854.2018.01.003

澳大利亚北卡那封盆地晚三叠世混合沉积特征

Mixed Carbonate-Siliciclastic Sedimentation of Upper Triassic in Northern Carnarvon Basin,Australia

黄众 1胡孝林 1杨松岭 1张璐1

作者信息

  • 1. 中海油研究总院
  • 折叠

摘要

Abstract

In Upper Triassic Brigadier Formation, there developed delta sandstone and mudstone in the southeast of Northern Carnarvon Basin, whereas developed carbonate rock in the northwest of the basin. According to some proofs of source input in the southeastern part of the basin, there developed siliciclastic sediments of delta facies near the provenance,and developed reef-shoal sediments and slump sediments away from the provenance. It is suggested that the mixed sedimentation in the Brigadier Formation is a typical facies mixing with carbonate rocks on the early fluvial sandstones,mainly due to the cessation of debris input and the reduction of hydrodynamic forces.

关键词

澳大利亚/北卡那封盆地/晚三叠世/Brigadier组/混合沉积/沉积模式

Key words

Late Triassic/Brigadier Formation/Mixed carbonate-siliciclastic sediments/Sedimentary model/Northern Carnarvon Basin/Australia

分类

能源科技

引用本文复制引用

黄众,胡孝林,杨松岭,张璐..澳大利亚北卡那封盆地晚三叠世混合沉积特征[J].海相油气地质,2018,23(1):21-28,8.

基金项目

本文受国家科技重大专项"海外重点区勘探开发关键技术"(编号:2017ZX05032)资助 (编号:2017ZX05032)

海相油气地质

OA北大核心CSCDCSTPCD

1672-9854

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