海相油气地质Issue(3)：66-72,7.DOI:10.3969/j.issn.1672-9854.2015.03.010
“源热共控”新西兰南大盆地生烃潜力
Hydrocarbon Generation Potential in Great South Basin, New Zealand
摘要
Abstract
Grea t South Basin has experienced three tectonic evolution stages, i.e. the rifting, the depression and the passive margin stages. Three set of source rocks developed in the basin, which are Hoiho Group coal-measures that formed during the rifting stage, and Taratu coastal plain coal-measures and Wickliffe marine mudstone that formed during the depression stage. In the light of Zhang′s "source-heat co-control" theory, it is indicated that Hoiho Group coal-measures should be the principle gas source rock owing to their deep burial and large effective volume with abundant organic matter and high thermal evolution. Besides Taratu coal-measures may be also effective source rock in local areas. It is believed that Central Depression where thick source rocks develop is of giant hydrocarbon potential.关键词
新西兰/南大盆地/烃源岩/生烃潜力/源热共控论Key words
Source rock/Hydrocarbon potential/Co-control of source and heat/Great South Basin/New Zealand分类
能源科技引用本文复制引用
金莉,杨松岭,柯岭,骆宗强,孙翠娟..“源热共控”新西兰南大盆地生烃潜力[J].海相油气地质,2015,(3):66-72,7.基金项目
本文受国家科技重大专项“大陆边缘盆地类比与油气成藏规律研究”（编号2011ZX05030001）资助 （）
