Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1306/0608171609417067 |
Burial and exhumation history of the Galilee Basin, Australia: Implications for unconventional hydrocarbon prospectivity | |
I&1; 39;Anson, Amy2 | |
2018-03-01 | |
发表期刊 | AAPG BULLETIN |
ISSN | 0149-1423 |
EISSN | 1558-9153 |
出版年 | 2018 |
卷号 | 102期号:3页码:483-507 |
文章类型 | Article |
语种 | 英语 |
国家 | Australia; England; Netherlands |
英文摘要 | This multidisciplinary study describes the burial and exhumation history of the frontier Galilee Basin in central Queensland, Australia, with implications for understanding its geohistory and unconventional gas prospectivity. Seismic interpretation, stratigraphic mapping, and an analysis of exhumation through quantifying overcompaction show total subsidence of approximately 2 km (similar to 6600 ft) from the Carboniferous to the Late Cretaceous, punctuated by two major exhumation events. Triassic exhumation was less than 600 m (< 1970 ft), whereas Late Cretaceous exhumation was in the order of 1000 m (3300 ft), increasing eastward to greater than 1600 m (5250 ft). Geohistory reconstructions show that Permian coal measures generated up to 45 m(3)/t (1590 ft(3)/t) of gas when modeled temperatures exceeded 100 degrees C (210 degrees F) during maximum burial of 1.5-2 km (4920-6560 ft) in the Late Cretaceous. In the Carboniferous to the mid-Cretaceous, the basin was situated to the west of the Eastern Australian subduction zone, where proto-Pacific oceanic lithosphere was subducted until circa 100 Ma, when subduction ceased. Our study shows that the geohistory of the basin is characterized by rapid subsidence of 50 m/m.y. (165 ft/m.y.) followed by rebound at circa 95 Ma resulting in an uplift and erosion phase. The undersaturation of the coals at present day is explained by this uplift event. Carbon isotopes indicate that the remaining gas (< 8 m(3)/t [< 280 ft(3)/t]) is of mixed biogenic and thermogenic origin. Therefore, dynamic surface topography driven by subduction dynamics and slab breakoff had a profound effect on the subsidence, uplift, and resource potential of the Galilee Basin. |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000430928900006 |
WOS关键词 | COAL-BED METHANE ; EASTERN AUSTRALIA ; VERTICAL MOTION ; SUBSIDENCE ; OXIDATION ; ORIGIN ; UPLIFT ; BOWEN ; SURAT ; GAS |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/24428 |
专题 | 地球科学 |
作者单位 | 1.Univ Sydney, Sch Geosci, Earthbyte Grp, Camperdown, NSW 2006, Australia; 2.TGS, Geol Prod & Serv Interpretat, 1 Crescent, Surbiton KT6 4BN, Surrey, England; 3.Shell Global Solut Int BV, Geosci, NL-2288 GS Rijswijk, Netherlands |
推荐引用方式 GB/T 7714 | I&,39;Anson, Amy. Burial and exhumation history of the Galilee Basin, Australia: Implications for unconventional hydrocarbon prospectivity[J]. AAPG BULLETIN,2018,102(3):483-507. |
APA | I&,&39;Anson, Amy.(2018).Burial and exhumation history of the Galilee Basin, Australia: Implications for unconventional hydrocarbon prospectivity.AAPG BULLETIN,102(3),483-507. |
MLA | I&,et al."Burial and exhumation history of the Galilee Basin, Australia: Implications for unconventional hydrocarbon prospectivity".AAPG BULLETIN 102.3(2018):483-507. |
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