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Anatomy of an obducted ultramafic unit (Tiébaghi Massif – Peridotite Nappe – New Caledonia): Polyphase brittle tectonics constrained by fault-slip data and crack seal mineralogy 一个断陷超基性单元(ti<s:1> baghi地块-橄榄岩推覆体-新喀里多尼亚)的解剖:受断滑数据和裂缝封闭矿物学约束的多期脆性构造
IF 2.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-08-14 DOI: 10.1080/00288306.2023.2243851
P. Maurizot, B. Robineau, J. Jeanpert, M. Iseppi, S. Lesimple, F. Juillot, Michael Meyer, Patrick Fullenwarth, V. Mardhel
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引用次数: 0
A tectonic reconstruction model for Aotearoa-New Zealand from the mid-Late Cretaceous to the present day 新西兰奥特亚白垩纪中晚期至今的构造重建模型
IF 2.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-08-02 DOI: 10.1080/00288306.2023.2239175
H. Seebeck, D. Strogen, A. Nicol, Benjamin R. Hines, K. J. Bland
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引用次数: 0
A possible Jurassic age for the New Caledonia Trough and implications for Zealandia’s history 新喀里多尼亚海槽可能的侏罗纪时代及其对西兰迪亚历史的影响
IF 2.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-07-19 DOI: 10.1080/00288306.2023.2232584
C. Uruski
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引用次数: 1
Sedimentation since 140 ka in Te Tai-o-Aorere Tasman Bay, Aotearoa New Zealand 新西兰奥特亚Te Tai-o-Orere Tasman湾140 ka以来的沉积
IF 2.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-07-12 DOI: 10.1080/00288306.2023.2229759
K. L. Maier, S. Woelz, P. Barnes, S. Nodder, A. Orpin, J. Mountjoy
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引用次数: 1
Records of the 5 March 2021 Raoul Island transoceanic tsunami around the Pacific Ocean 2021年3月5日太平洋周边拉乌尔岛跨洋海啸记录
IF 2.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-07-04 DOI: 10.1080/00288306.2023.2225859
J. Roger
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引用次数: 1
Roger Cooper: paleobiologist and geologist 罗杰·库珀:古生物学家和地质学家
IF 2.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.1080/00288306.2023.2236308
J. Crampton, R. Jongens, A. Cooper
Roger Cooper (1939–2020) was one of the pre-eminent New Zealand paleontologists and geologists of the twentieth century. As with many scientists of his generation, he developed a broad suite of skills and his research ranged widely – a testament to his talents but also a function of the small number of Earth scientists studying New Zealand’s complex geology. Although he always understood that science builds on a foundation of careful observation and description – and he made huge contributions in this regard – he also sought and applied innovative analytical approaches. Roger was open, kind and generous as a mentor, colleague, collaborator and manager. The present collection of papers pays homage to the many ways that Roger’s research advanced understanding of Zealandia’s geological history and wider questions in paleobiology, and several of these papers are written by people whose careers were enriched by their interactions with Roger. Accurate and precise field observation underpins much of Earth science. Roger knew this, but for him field work was also an opportunity to rejuvenate mind and body and immerse himself in the living world; his joy of life always shone brightest when he was in the field. As a second-year geology undergraduate student at Victoria University of Wellington, he was fortunate to join Gerald Lensen of the New Zealand Geological Survey (now GNS Science) for a threemonth expedition to produce a geological map of the Clarence valley area in the South Island (Lensen 1962). The field work was challenging but hugely educational for Roger; in his own, understated words, ‘I was a pretty raw second year student when we started and learned a lot from the experience’ (Roger Cooper, written pers. comm. 2017; see obituary by Crampton, Beu, et al. 2020a). The paper herein by Crampton (2023) revisits the geology of the northern Clarence valley area, covering a small part of the territory mapped by Roger, and uses new observations of field relationships to interpret the Cretaceous tectonostratigraphic history; these new data bear on the contentious issue of exactly when Mesozoic subduction terminated on the margin of Gondwana. By the time he had finished his PhD, supervised by Harold Wellman, Roger had completed field seasons in the Antarctic, Otago, Southland, and the Golden Bay area, and had spent 18 months on the island of Borneo (Crampton, Beu, et al. 2020). His growing family joined him for field work in the Golden Bay area, based in Magnesite Hut in the Cobb valley. Helicopter trips to remote ridges, caves full of moa bones, and mountain lakes and streams kept children happy and formed their long-lasting affinities with the New Zealand bush and upland country. Roger’s Borneo jungle experience equipped him with a range of distinctive long-distance bush communication calls, his faithful parang (a type of machete made from a car leaf spring), and the ability to make a fire under any conditions, all of which translated well to New Zeal
罗杰·库珀(1939-2020)是20世纪新西兰最杰出的古生物学家和地质学家之一。和他那一代的许多科学家一样,他发展了一套广泛的技能,他的研究范围也很广——这是他才华的证明,但也是为数不多的研究新西兰复杂地质的地球科学家的作用。尽管他始终明白科学建立在仔细观察和描述的基础上——他在这方面做出了巨大贡献——但他也寻求并应用了创新的分析方法。作为导师、同事、合作者和经理,罗杰是开放、善良和慷慨的。本书收录的论文从多方面向罗杰的研究致敬,这些研究促进了人们对西兰迪亚地质历史和更广泛的古生物学问题的理解,其中一些论文的作者因与罗杰的互动而丰富了他们的事业。精确的野外观测是地球科学的基础。罗杰知道这一点,但对他来说,野外工作也是一个恢复身心活力、让自己沉浸在现实世界中的机会;当他在田间时,他的生活乐趣总是闪耀着最耀眼的光芒。作为惠灵顿维多利亚大学地质学本科二年级的学生,他很幸运地加入了新西兰地质调查局(现在的GNS科学)的Gerald Lensen,进行了为期三个月的考察,绘制了南岛克拉伦斯山谷地区的地质图(Lensen 1962)。实地工作很有挑战性,但对罗杰来说很有教育意义;用他自己轻描淡写的话说,刚开始的时候,我是一个非常不成熟的二年级学生,从这次经历中学到了很多东西。通讯。2017;参见Crampton, Beu等人的讣告。2020a)。Crampton(2023)的论文重新审视了克拉伦斯河谷北部地区的地质情况,覆盖了Roger绘制的一小部分领土,并使用新的野外关系观测来解释白垩纪构造地层历史;这些新资料对中生代俯冲作用何时终止于冈瓦纳边缘这一有争议的问题产生了影响。在Harold Wellman的指导下完成博士学位时,Roger已经完成了在南极、奥塔哥、南地和金湾地区的实地考察,并在婆罗洲岛度过了18个月(Crampton, Beu, et al. 2020)。他不断壮大的家庭加入了他在金湾地区的实地工作,总部设在科布山谷的菱镁矿小屋。乘坐直升机前往偏远的山脊、满是恐鸟骨头的洞穴、山上的湖泊和溪流,让孩子们感到快乐,并与新西兰的丛林和高地国家形成了长期的亲密关系。罗杰在婆罗洲丛林的经历使他具备了一系列独特的远距离丛林交流呼叫,他忠实的parang(一种由汽车钢板弹簧制成的弯刀),以及在任何条件下生火的能力,所有这些都很好地转化为新西兰的野外工作。每天结束漫长的一天后,他会在晒伤处大量涂抹甲基化烈酒,并与同事和学生一起畅饮一杯老穆泰尔苹果酒。他的儿子艾伦回忆说,他曾多次停下来检查道路切割,当他在上奥陶世的砂岩中(在科布山谷的路上)意外地发现了珊瑚之类的东西时,他几乎无法抑制自己的兴奋,这让他觉得很有价值,这也激发了艾伦对实地科学的热情。罗杰在新西兰地质调查局的职业生涯始于1969年,最初专注于新西兰早期古生代化石的分类学、生物地层学、进化、生物地理学和古生物学。这些研究大多与笔石有关(如Cooper 1973,1979a;但在与其他人的合作下,他的兴趣迅速扩大到包括来自新西兰、澳大利亚、南极洲和斯匹次卑尔根岛的牙形刺、腕足动物、软体动物、三叶虫和笔石(例如Cooper and Druce 1975;Shergold et al. 1976)。罗杰职业生涯的一个标志是他与世界各地的科学家建立了终生的合作和友谊。一个早期的例子
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引用次数: 0
The Ross–Delamerian Orogen in the southwest Pacific and Antarctica: an active plate boundary for Gondwana in the late Neoproterozoic and Cambrian 西南太平洋和南极洲的Ross–Delamerian造山带:新元古代晚期和寒武纪冈瓦纳大陆的活动板块边界
IF 2.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.1080/00288306.2023.2236049
J. Bradshaw
ABSTRACT Neoproterozoic and Cambrian tectonic and magmatic events in southeast Australia, Tasmania, New Zealand and the Transantarctic Mountains have been described as aspects of the Ross–Delamerian Orogeny. Summaries of the salient points suggest they are parts of the same active margin that developed along a paleo-Pacific rifted edge of the fragmented Rodinia supercontinent. Late Neoproterozoic to Cambrian subduction produced a major magmatic arc that cuts Neoproterozoic and early Cambrian rocks. The Ross–Delamerian Orogen includes two exotic blocks, the Beardmore and VanDieland microcontinents, which accreted in the early Cambrian and middle Cambrian respectively. Other possible exotic elements are the Bowers Terrane in northern Victoria Land and the Takaka Terrane in New Zealand, with both sharing a common middle to late Cambrian history. Compressive deformation occurred at poorly constrained intervals in the early Cambrian but is well constrained in the middle Cambrian. In Australia and Victoria Land of Antarctica, magma compositions changed in the late Cambrian reflecting a change to extension. Bi-modal volcanism and stratigraphy in the Pensacola Mountains of Antarctica are similarly interpreted. Subduction slowed and ceased towards the end of the Cambrian implying a change in relative motion along the Australian–Antarctica segment of the Gondwanan plate boundary.
摘要澳大利亚东南部、塔斯马尼亚、新西兰和跨南极山脉的新元古代和寒武纪构造和岩浆事件被描述为罗斯-德拉梅里造山运动的一部分。突出点的总结表明,它们是沿着支离破碎的罗迪尼亚超大陆的古太平洋裂谷边缘发育的同一活动边缘的一部分。新元古代晚期到寒武纪的俯冲产生了一个主要的岩浆弧,切割新元古代和寒武纪早期的岩石。Ross–Delamerian造山带包括两个奇异地块,Beardmore和VanDieland微大陆,它们分别在早寒武纪和中寒武纪增生。其他可能的外来元素包括维多利亚地北部的鲍尔斯阶地和新西兰的塔卡阶地,两者都有着共同的寒武纪中晚期历史。在寒武纪早期,压缩变形发生在约束较差的区间,但在寒武纪中期受到很好的约束。在澳大利亚和南极洲的维多利亚地,晚寒武纪的岩浆成分发生了变化,反映了伸展的变化。对南极洲彭萨科拉山脉的双峰火山活动和地层学进行了类似的解释。俯冲在寒武纪末期减缓并停止,这意味着冈瓦纳板块边界的澳大利亚-南极洲段的相对运动发生了变化。
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引用次数: 1
Basanite cobbles in Pleistocene sediments in Central Otago and their implications for intraplate volcanism and Clutha River paleo-drainage 奥塔哥中部更新世沉积物中的蓝晶石鹅卵石及其对板内火山活动和Clutha河古水系的影响
IF 2.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-06-15 DOI: 10.1080/00288306.2023.2224579
J. Scott, A. Cooper, D. Craw, P. L. le Roux, H. Dalton, M. Palmer
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引用次数: 1
Tectonic subsidence and uplift within Canterbury Basin, South Island, New Zealand 新西兰南岛坎特伯雷盆地的构造沉降和隆起
IF 2.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-06-07 DOI: 10.1080/00288306.2023.2214368
K. Dvořák, M. Kominz, M. Crundwell
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引用次数: 0
Composition and Miocene deformation of the lithospheric mantle adjacent to the Marlborough Fault System in North Canterbury 北坎特伯雷Marlborough断层系附近岩石圈地幔的组成和中新世变形
IF 2.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-06-04 DOI: 10.1080/00288306.2023.2218101
Sophie J. Bonnington, J. Scott, M. Palmer, Nadine P. Cooper, M. Reid, C. Stirling
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引用次数: 1
期刊
New Zealand Journal of Geology and Geophysics
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