Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1306/0206181616817222 |
Geochemical, petrographic, and uranium-lead geochronological evidence for multisourced polycyclic provenance of deepwater strata in a hybrid tectonic setting: The upper Miocene upper Mount Messenger Formation, Taranaki Basin, New Zealand | |
Rotzien, Jonathan R.1; Browne, Greg H.2; King, Peter R.2 | |
2018-09-01 | |
发表期刊 | AAPG BULLETIN |
ISSN | 0149-1423 |
EISSN | 1558-9153 |
出版年 | 2018 |
卷号 | 102期号:9页码:1763-1802 |
文章类型 | Article |
语种 | 英语 |
国家 | USA; New Zealand |
英文摘要 | Petrographic, detrital zircon, major, trace, and rare earth element data from the deep-water slope upper Miocene upper Mount Messenger Formation, Taranaki Basin, New Zealand have been characterized to examine their provenance, tectonic setting, grain size, and source-to-sink implications. Sandstone samples have an average quartz-feldspar-lithic framework composition of Q(37)F(9)L(54). Lithic fragments are metasedimentary and commonly quartz and epidote bearing, having been recycled through at least two phases of erosion and deposition from an original orogenic to transitional arc setting. Detrital zirconU-Pb ages (total 304 single-grain ages) range from 37 to 2466 Ma, with large Triassic to Permian modes and small mid-Cretaceous, Early Jurassic, Devonian-Ordovician, Cambrian, and Proterozoic modes. The ages show subtle variation from the base to the top of the formation and statistical similarity with the Torlesse composite terrane and Waipapa Group. Trace and rare earth element analyses indicate enrichment in Th and Zr compared with Sc and Cr, and a strong Eu anomaly. The depositional system is over-whelmingly fine-to very fine-grained and probably reflects grain recycling andmechanical breakdown, either through an intermediate depositional cycle or derived directly from metasedimentary basement sources. Basement sources appear to be primarily the Torlesse composite terrane (Rakaia, Pahau, and Kaweka terranes) and Waipapa Group located east and southeast of the study area. This study documents source-to-sink elements in a profoundly regressive depositional system within an active margin setting. It also contributes new information on the composition and depositional history of a stratigraphic interval that contains important petroleum reservoirs in the nearby subsurface. |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000445705200005 |
WOS关键词 | DETRITAL-ZIRCON AGES ; FORE-ARC BASIN ; NORTHERN NORTH-ISLAND ; BROOK STREET TERRANE ; SOUTH-ISLAND ; TORLESSE TERRANE ; MARLBOROUGH SCHIST ; STRATIGRAPHIC ARCHITECTURE ; GONDWANA MARGIN ; ISOTOPIC CHARACTERIZATION |
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/24530 |
专题 | 地球科学 |
作者单位 | 1.Basin Dynam, 1875 Post Oak Pk Dr, Houston, TX 77027 USA; 2.Inst Geol & Nucl Sci, 1 Fairway Dr, Lower Hutt 5040, New Zealand |
推荐引用方式 GB/T 7714 | Rotzien, Jonathan R.,Browne, Greg H.,King, Peter R.. Geochemical, petrographic, and uranium-lead geochronological evidence for multisourced polycyclic provenance of deepwater strata in a hybrid tectonic setting: The upper Miocene upper Mount Messenger Formation, Taranaki Basin, New Zealand[J]. AAPG BULLETIN,2018,102(9):1763-1802. |
APA | Rotzien, Jonathan R.,Browne, Greg H.,&King, Peter R..(2018).Geochemical, petrographic, and uranium-lead geochronological evidence for multisourced polycyclic provenance of deepwater strata in a hybrid tectonic setting: The upper Miocene upper Mount Messenger Formation, Taranaki Basin, New Zealand.AAPG BULLETIN,102(9),1763-1802. |
MLA | Rotzien, Jonathan R.,et al."Geochemical, petrographic, and uranium-lead geochronological evidence for multisourced polycyclic provenance of deepwater strata in a hybrid tectonic setting: The upper Miocene upper Mount Messenger Formation, Taranaki Basin, New Zealand".AAPG BULLETIN 102.9(2018):1763-1802. |
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