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Aspidella and water escape structures from the ca 850 Ma (Tonian) Heavitree Formation, Amadeus Basin, Central Australia 澳大利亚中部 Amadeus 盆地约 850 Ma(托尼安纪)Heavitree 地层中的 Aspidella 和水逸结构
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-12-18 DOI: 10.1080/08120099.2023.2290248
P. S. Plummer, J. D. Gorter
The mid-Tonian-aged Heavitree Formation, the basal unit of the Amadeus Basin succession, has long been believed to be devoid of metazoan fossils. Since a recent review of isolated occurrences of pu...
中唐时代的海维特里地层是阿玛迪斯盆地演替的基底单元,长期以来一直被认为没有元古宙化石。自从最近对个别出现的古脊椎动物化石进行了审查之后,该化石被认为是一种非常罕见的化石。
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引用次数: 0
The Tasmanian Tyennan Domain–a structural synthesis and review with tectonic and dynamic implications for continental margin subduction and exhumation 塔斯马尼亚泰南岩域--结构综述和回顾,以及对大陆边缘俯冲和掘起的构造和动力学影响
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-12-06 DOI: 10.1080/08120099.2023.2280604
David Ross Gray, M. J. Vicary, A. W. McNeill
The Tyennan Domain of western Tasmania is a structurally emplaced, complexly deformed lithotectonic sheet (allochthon). It comprises stacked, isoclinally folded slabs of allochthonous high-grade sc...
塔斯马尼亚州西部的泰南岩域是一个构造隆起、变形复杂的岩石构造板块(allchthon)。它由堆叠、等轴褶皱的高品位全岩...
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引用次数: 0
Outcrop to petrography scale and new age constraint of the Jatisamit Mélange in the Luk Ulo area, Central Java, Indonesia 印度尼西亚中爪哇 Luk Ulo 地区 Jatisamit Mélange 的外露规模和岩相尺度及新年龄约束
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-12-06 DOI: 10.1080/08120099.2023.2273419
M. Z. Tuakia, Rendy, W. D. Santoso, E. Puswanto, F. S. Yuwono, B. Sapiie, A. Dianto
To resolve the formation of the Luk Ulo Mélange in the Karangsambung area of Central Java, the matrix-dominated Jatisamit Mélange, which is a member of the Luk Ulo Mélange, was examined. Outcrop an...
为了解决中爪哇 Karangsambung 地区 Luk Ulo Mélange 的形成问题,我们考察了以基质为主的 Jatisamit Mélange,它是 Luk Ulo Mélange 的一个成员。该岩层的露头和...
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引用次数: 0
Shoshonitic pluton and an associated base-metal deposit in the Tarom–Hashtjin metallogenic zone, NW Iran: implication for tectono-magmatic evolution and metallogenic considerations 伊朗塔罗姆-哈什金成矿带shoshonic岩体及其伴生贱金属矿床:构造-岩浆演化及成矿意义
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-12-04 DOI: 10.1080/08120099.2023.2273974
M. Afshari, Gh. Nabatian, M. Honarmand, M. Ebrahimi, X-H. Li
Petrological, geochemical and zircon U–Pb and Hf isotope studies were carried out on the Hajseyran pluton, along the Tarom–Hashtjin metallogenic zone, as part of the Alborz–Azerbaijan magmatic belt...
对沿Tarom-Hashtjin成矿带(Alborz-Azerbaijan岩浆带的一部分)的Hajseyran岩体进行了岩石学、地球化学和锆石U-Pb和Hf同位素研究。
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引用次数: 0
Paleogene carbonate ramp development in the Kohat Basin of northwestern Pakistan 巴基斯坦西北部科哈特盆地古近系碳酸盐岩斜坡发育
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-29 DOI: 10.1080/08120099.2023.2279062
S. Ahmad, D. Kroon, J. J. G. Reijmer, S. Khan, O. S. Hersi, B. Wadood
A series of well-exposed Paleogene sedimentary successions in the Kohat Basin of northwestern Pakistan (western Himalayas), are used to document the development of Paleogene sedimentary sequence de...
利用巴基斯坦西北部(喜马拉雅山脉西部)科哈特盆地一系列暴露良好的古近系沉积序列,研究了古近系沉积序列的发育。
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引用次数: 0
Reply to Discussion of Yule, C. T. G., Daniell, J., Edwards, D. S., Rollet, N., & Roberts, E. M. (2023). Reconciling the onshore/offshore stratigraphy of the Canning Basin and implications for petroleum prospectivity. Australian Journal of Earth Sciences, 70(5), 691–715 对Yule, c.t.g, daniel, J., Edwards, D. S, Rollet, N., and Roberts, E. M.(2023)讨论的答复。康宁盆地陆海地层调和及其油气远景意义地球科学进展,30 (5),691-715
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-27 DOI: 10.1080/08120099.2023.2269564
C. T. G. Yule, J. Daniell, D. S. Edwards, N. Rollet, E. M. Roberts
Published in Australian Journal of Earth Sciences: An International Geoscience Journal of the Geological Society of Australia (Vol. 70, No. 8, 2023)
发表于《澳大利亚地球科学杂志:澳大利亚地质学会国际地球科学杂志》(第70卷,第8期,2023年)
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引用次数: 0
Discussion of Yule, C.T.G., Daniell, J., Edwards, D.S., Rollet, N. & Roberts, E.M. (2023). Reconciling the onshore/offshore stratigraphy of the Canning Basin and implications for petroleum prospectivity. Australian Journal of Earth Sciences, 70(5), 691–715 讨论Yule, c.t.g., daniel, J., Edwards, d.s., Rollet, N. & Roberts, E.M.(2023)。康宁盆地陆海地层调和及其油气远景意义地球科学进展,30 (5),691-715
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-27 DOI: 10.1080/08120099.2023.2269572
A. J. Mory
Published in Australian Journal of Earth Sciences: An International Geoscience Journal of the Geological Society of Australia (Vol. 70, No. 8, 2023)
发表于《澳大利亚地球科学杂志:澳大利亚地质学会国际地球科学杂志》(第70卷,第8期,2023年)
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引用次数: 1
Subsurface high-grading potential in Coal Seam Gas in eastern Australia 澳大利亚东部煤层气地下高品位潜力
IF 1.2 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-19 DOI: 10.1080/08120099.2023.2271547
A. J. W. Everts, L. D. Alessio, C. J. Connell
A case study from eastern Australia is used to demonstrate methods for subsurface high-grading and development-concept optimisation in Coal Seam Gas resource plays. We discuss two aspects of subsur...
以澳大利亚东部的一个案例研究为例,展示了煤层气资源区地下高品位和开发理念优化的方法。我们从两个方面讨论亚…
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引用次数: 0
Tsunami or storm? A high-level coastal boulder field on the southern tip of Eyre Peninsula, South Australia 海啸还是风暴?位于南澳大利亚艾尔半岛南端的高水平海岸巨石场
4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-11-02 DOI: 10.1080/08120099.2023.2272678
R. P. Bourman, C. V. Murray-Wallace, D. Panda, S. Buckman, D. Banerjee, D. D. Ryan, L. T. White
A high-level coastal boulder field at Whalers Way, southern Eyre Peninsula, South Australia, occurs at elevations of 20–30 m above present sea-level on a gently seaward-sloping, karst-weathered calcrete-capped structural bench, formed on the Upper Pleistocene Bridgewater Formation and underlying Carnot Gneisses (Archean–Paleoproterozoic Sleaford Complex). More than 1000 ex situ boulders, cobbles and pebbles of gneiss and mafic igneous rocks, as well as fragments of calcrete, occur within the boulder field and cover an area >6000 m2. All the crystalline rock clasts are derived locally from bedrock outcrops along the adjacent coastline, where metasedimentary granulite-facies of the Carnot Gneisses crop out along shore platforms and their backing cliffs, close to present sea-level. The boulder field is younger than Marine Isotope Sub-Stage 5a (MIS 5a; ca 80 ka) based on amino acid racemisation ‘whole-rock’ analyses of calcarenite of the Bridgewater Formation, which forms the calcrete bench on which the boulder field rests. The boulder field wraps around the western extremity of cliff-top dunes dated at 18–17 ka by optically stimulated luminescence, implying that the boulder deposit post-dates the formation of the cliff-top dunes. Given that the clasts in the boulder field show minimal weathering rinds, sea-level during the Last Glacial Maximum was some 125 m lower than present and that between 80 and 7 ka ago, sea-level never attained present levels within the region, emplacement of the boulder field by a high-energy wave event in the Holocene highstand, following the 7000 years BP culmination of post-Glacial sea-level rise, is suggested. Storm waves, rather than a tsunami, most likely explain the emplacement of the boulder field.
南澳大利亚Eyre半岛南部的Whalers Way有一个高水平的海岸巨石场,位于海拔20-30米的海面上,形成于上更新世Bridgewater组和卡诺片岩(太古宙-古元古代Sleaford杂岩)下的一个缓慢向海倾斜的岩溶风化钙质盖层构造台地。在巨石场内,有1000多个片麻岩和基性火成岩的非原位巨石、鹅卵石和鹅卵石,以及钙质碎片,占地面积超过6000平方米。所有的结晶岩石碎屑都来自邻近海岸线的基岩露头,卡诺片麻岩的变质沉积岩麻粒岩相沿着海岸台地及其背后的悬崖生长,接近现在的海平面。岩石田比海洋同位素5a亚阶段(MIS 5a)年轻;大约80 ka),基于桥水组钙砾岩的氨基酸外消旋“全岩”分析,桥水组形成了巨石场所在的钙砾岩台阶。根据光激发光法测定,崖顶沙丘的形成时间为18 ~ 17 ka,在其西端包裹着砾石场,表明该砾石沉积时间晚于崖顶沙丘的形成。考虑到末次盛冰期的海平面比现在低125 m,而80 ~ 7 ka以前,该地区的海平面从未达到现在的水平,因此,在距今7000年的冰期后海平面上升高潮之后,全新世高地发生了一次高能波事件,导致了巨石场的就位。风暴波,而不是海啸,最有可能解释巨石场的位置。
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引用次数: 0
Geodynamic evolution in the post-collisional stage of the East Kunlun Orogenic Belt: constraints from the Late Triassic intermediate–felsic igneous rocks 东昆仑造山带碰撞后的地球动力学演化:来自晚三叠世中英质火成岩的约束
4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-10-23 DOI: 10.1080/08120099.2023.2263883
A-K. Zhang, S-Y. He, Y. Zhang, J-L. Sun, Y. Qian
AbstractThe Late Triassic igneous rocks associated with post-collision are widely distributed in the East Kunlun Orogenic Belt (EKOB), but their specific dynamic mechanism and evolutional process are still controversial. To address these key issues, we investigated the geochronology and geochemistry of intermediate–felsic igneous rocks from the EKOB, including trachyandesite, rhyolite, porphyritic monzogranite, syenogranite, granite porphyry and crystalline tuff. Zircon U–Pb isotopes of these rocks indicate that they were formed between 231.1 and 215.8 Ma (i.e. Late Triassic). These igneous rocks have moderate to high SiO2 (60.29–79.56 wt%) and low mantle compatible element contents (e.g. Co: 0.37–12.62 ppm; Ni: 1.55–15.59 ppm), suggesting that continental crustal-derived material played an important role in their formation. Porphyritic monzogranite (231.1 Ma), syenogranite (228.1 Ma), trachyandesite (227.4 Ma) and rhyolite (215.8 Ma) have Nb/U (1.41–4.71) and Ce/Pb (1.48–6.19) ratios like that of the crust, with εHf(t) values (–1.31 to 2.26) and old two-stage model (TDM2) ages of 1340–1119 Ma, suggesting that they originated from the partial melting of a Mesoproterozoic crust with minor mantle material involved in their source. Crystalline tuff (224.6 Ma) and granite porphyry (222.3 Ma) have Nb/U (1.93–3.81) and Ce/Pb (0.30–3.18) ratios, negative εHf(t) values (–7.04 to −5.12) and old TDM2 ages (1703–1581 Ma) closer to those of crust, suggesting that they were derived from the partial melting of a Paleo–Mesoproterozoic continental crust without addition of mantle material. Based on our new data and published data, the Late Triassic igneous rocks from the EKOB can be divided into three stages, 236–227, 226–218 and 216–208 Ma, corresponding to slab break-off, lithospheric mantle delamination and thickened lower crust delamination, respectively.KEY POINTSThe intermediate–felsic igneous rocks from the East Kunlun Orogenic Belt are dated from 231.1 to 215.8 Ma (i.e. Late Triassic).These igneous rocks were derived from the partial melting of ancient continental crust.The Late Triassic igneous rocks from the East Kunlun Orogenic Belt can be divided into three stages, including slab break-off, lithospheric mantle delamination and thickened lower crust delamination.Keywords: East Kunlun Orogenic BeltLate Triassicpost-collisional magmatismgeodynamic evolutionintermediate–felsic igneous rocksslab break-offdelamination Data availability statementThe authors confirm that the data supporting the findings of this study are available within the article and the Supplemental data.Disclosure statementNo potential conflict of interest was reported by the author(s).Additional informationFundingThis research was funded by the Key Research Program of the National Natural Science Foundation of China (92062217), the Kunlun Talents High-end Innovative and Entrepreneurial Talents Project of Qinghai Province ([2022] No. 32), the Science and Technology Project of Qinghai Pr
摘要东昆仑造山带广泛分布有晚三叠世后碰撞伴生火成岩,但其具体的动力机制和演化过程仍存在争议。为了解决这些关键问题,我们研究了EKOB中长英质火成岩的年代学和地球化学,包括粗面山岩、流纹岩、斑状二长花岗岩、正长花岗岩、花岗斑岩和结晶凝灰岩。锆石U-Pb同位素表明,这些岩石形成于231.1 ~ 215.8 Ma(晚三叠世)之间。这些火成岩具有中高SiO2 (60.29-79.56 wt%)和低地幔相容元素含量(如Co: 0.37-12.62 ppm);Ni: 1.55 ~ 15.59 ppm),表明大陆地壳源物质在其形成过程中起了重要作用。斑岩型二长花岗岩(231.1 Ma)、正长花岗岩(228.1 Ma)、粗长山岩(227.4 Ma)和流纹岩(215.8 Ma)的Nb/U(1.41 ~ 4.71)和Ce/Pb(1.48 ~ 6.19)比值与地壳相似,εHf(t)值为-1.31 ~ 2.26,两阶段模式(TDM2)年龄为1340 ~ 1119 Ma,表明它们起源于中元古代地壳的部分熔融,来源中地幔物质较小。结晶凝灰岩(224.6 Ma)和花岗岩斑岩(222.3 Ma)的Nb/U(1.93 ~ 3.81)和Ce/Pb(0.30 ~ 3.18)比值,εHf(t)值为负(-7.04 ~ - 5.12),TDM2年龄(1703 ~ 1581 Ma)较接近地壳年龄,表明它们来源于古-中元古代大陆地壳的部分熔融,没有地幔物质的加入。根据新资料和已有资料,鄂西坳陷晚三叠世火成岩可划分为236 ~ 227 Ma、226 ~ 218 Ma和216 ~ 208 Ma三个阶段,分别对应于板块断裂、岩石圈地幔剥离和下地壳增厚剥离。东昆仑造山带的中长英质火成岩年龄为231.1 ~ 215.8 Ma(即晚三叠世)。这些火成岩是古代大陆地壳部分熔融形成的。东昆仑造山带晚三叠世火成岩可分为板块断裂、岩石圈地幔剥离和下地壳增厚剥离3个阶段。关键词:东昆仑造山带晚三叠世碰撞后岩浆地球动力学演化中英质火成岩岩裂脱层数据可用性声明作者在文章和补充资料中确认了支持本研究结果的数据。披露声明作者未报告潜在的利益冲突。本研究由国家自然科学基金重点研究项目(92062217)、青海省昆仑英才高端创新创业人才项目([2022]32号)、青海省科技计划项目(2019-ZJ-7009)、青海省昆仑英才高端创新创业人才项目([2021]16号)资助。
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Australian Journal of Earth Sciences
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