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Emplacement processes of ignimbrites in the Ongatiti Valley, southeast Te Kuiti

机译:蒂奎蒂东南部昂加蒂蒂河谷中火成岩的成藏过程

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摘要

The Mangakino volcanic centre (MVC) is the oldest rhyolitic volcano of the Taupo Volcanic Zone (TVZ) located on the westernmost boundary. Ten eruptive deposits have been derived from the MVC and this study focuses on the 1.21 ± 0.04 Ma Ongatiti Ignimbrite and the 1.20 ± 0.04 Ma Unit D fall and overlying ignimbrite deposit. The Taupo volcanic centre (TVC), located at the southern boundary of the central TVZ is currently active and is considered to be the most active and productive rhyolitic centre on Earth. There have been multiple eruptions derived from the TVC over the past 350 – 320 ka, however the most recent Taupo eruption dated at 232 AD is the only deposit studied in this research. The study area is situated within the Ongatiti Valley, 15 km SE of Te Kuiti. It is 28 km west of the Mangakino caldera rim, and is located to the west of the upstanding Mesozoic basement block of the Rangitoto Range. A 1:25 000 geological map of the volcanic geology exposed within the Ongatiti Valley is produced. Detailed stratigraphc logs, petrographic descriptions and quantitative analysis on the mineralogy are given for all of the exposed eruptive deposits. The geochemical composition of the Ongatiti Ignimbrite and Unit D are determined through XRF, Electron microprobe and ICPMS analyses. Stratigraphic sections of the Ongatiti Ignimbrite in well exposed 25 m high outcrops in the Ongatiti Valley show variations in pumice, crystal, and lithic abundance, both vertically and laterally. Two units can be distinguished within the Ongatiti Ignimbrite overlying a poorly exposed lowermost fall deposit: a lower densely to partially welded, crystal-rich, pumice-poor flow sequence, and an upper densely to partially welded pumice and crystal-rich flow sequence. The boundary between the two units is wavy and gradational, and varies in altitude over relatively short distances. This undulating boundary is considered to result from interaction of pyroclastic density currents flowing both over and around the high-standing Rangitoto Range, and then covering a highly irregular pre-ignimbrite topography in the King Country. In the Ongatiti Valley, Unit D consists of several phreatoplinian fall deposits, a fine-grained ignimbrite and an overlying coarser-grained ignimbrite with a combined thickness of 3 m. A stratigraphic log is presented and the characteristic textures, structure, petrography and geochemistry is described. A six stage process is suggested for the change in the conditions/styles and intensities between the different phases of the eruption. A 15 m high valley-ponded section of the 232 AD Taupo Ignimbrite occurs in the Waipa River Valley, that contains fossilised tree trunks in position of growth. A possible origin involving variation in dynamic pressure and subsequent destructive power of pyroclastic density currents is developed.
机译:芒甘基诺火山中心(MVC)是位于最西边界的陶波火山带(TVZ)中最古老的流纹火山。 MVC派生了10个喷发沉积物,该研究的重点是1.21±0.04 Ma的Ongatiti着火岩和1.20±0.04 Ma的D单元降落和上覆的火成岩沉积物。位于中央TVZ南部边界的陶波火山中心(TVC)目前处于活跃状态,被认为是地球上最活跃,生产力最高的流纹岩中心。在过去的350 – 320 ka期间,TVC曾发生过多次喷发,但是最新的陶波喷发始于公元232年,是该研究中唯一研究的矿床。研究区域位于Te Kuiti东南15公里处的Ongatiti山谷内。它位于Mangakino火山口边缘以西28公里,位于朗伊托托山脉直立的中生代地下室地块的西部。绘制了Ongatiti山谷内暴露的火山地质的1:25 000地质图。针对所有裸露的喷出矿床,提供了详细的地层测井,岩石学描述和矿物学定量分析。通过XRF,电子探针和ICPMS分析确定Ongatiti着火岩和D单元的地球化学组成。在Ongatiti山谷中暴露良好的25 m高露头中的Ongatiti火山岩地层剖面在垂直和横向上都显示出浮石,晶体和石屑丰度的变化。在Ongatiti Ignimbrite中,可以区分出两个单元,它们覆盖在暴露程度最差的最低秋天沉积物上:较低的稠密到部分焊接的,富含晶体的浮石,流动顺序较低,以及较高的稠密到部分焊接的浮石和富含晶体的流序。两个单元之间的边界是波浪形和渐变的,并且在相对较短的距离内高度会发生变化。这种起伏的边界被认为是由高温碎屑密度流相互作用的结果,这些碎屑密度流流过高耸的朗伊托托山脉及其周围,然后覆盖了金国的高度不规则的着火前地貌。在Ongatiti山谷中,D单元由几个phareatoplinian秋季沉积物,一个细颗粒的火成岩和一个上覆的较粗颗粒的火成岩组成,总厚度为3 m。给出了地层测井资料,并描述了特征构造,结构,岩石学和地球化学。对于喷发不同阶段之间的条件/样式和强度的变化,建议采用六个阶段的过程。怀帕河谷发生在232 AD Taupo Ignimbrite的一个高15 m的山谷缓和部分,其中包含处于生长位置的化石树干。可能的起源涉及动压变化和火山碎屑密度电流的随后破坏力。

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    Brink Megan Tracy;

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  • 年度 2012
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