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Late Mesozoic ductile deformation and exhumation along the Shangdan suture zone in the Qinling Orogenic Belt, China 中国秦岭造山带上丹缝合带中生代晚期韧性变形与隆升
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-08-22 DOI: 10.1002/gj.5037
Le Zhang, Wei Li, Dazhi Jiang, Li Liang, Liuqing Jiang, Chao Wang, Zhenwei Feng, Zhihao Ma, Falak Sheir
The Qinling Orogenic Belt (QOB) is a multi‐stage orogenic belt recording subduction and collision processes. The ductile shearing deformation with different properties and ages is developed on the boundary of the different litho‐tectonic units, which can be used to decipher the tectonic evolution of the QOB. Previous studies mainly concentrated on the pre‐Late Mesozoic shearing deformation, while the Late Mesozoic shearing deformation received less attention. It restricts the understanding of the Late Mesozoic tectonic evolution of the QOB. Hence, we conducted detailed field structural analysis and laboratory analysis of the Shagou shear zone (SGSZ) in the middle part of the Shangdan suture zone (SDSZ). The SGSZ, developed in the southern margin of the Baliping pluton, is an S–SSW‐dipping sinistral strike‐slip ductile shear zone with a top‐to‐the‐ESE shear sense. The mylonite protoliths are voluminous Late Triassic granites (200–215 Ma) and a small amount of Neoproterozoic granites (759 Ma) and Early Cretaceous granites (145 Ma). Microstructures and geothermobarometer results suggest that the ductile shearing deformation occurred under high greenschist–low amphibolite‐facies conditions (400–650°C) at middle crustal depths (13–21 km). Zircon U–Pb and amphibole‐biotite 40Ar/39Ar dating results constrain the timing of shearing deformation to 135–145 Ma and the rapid exhumation of the SGSZ to 115–135 Ma. Combining with the regional data, we consider that the sinistral strike‐slip shearing deformation in the SGSZ controls and accommodates the south‐eastward extrusion of the East SQB under the intracontinental compression. Subsequently, the intracontinental extension led to the rapid exhumation of the SGSZ.
秦岭造山带是一个记录了俯冲和碰撞过程的多期造山带。在不同岩石构造单元的边界上发育着不同性质和时代的韧性剪切变形,可用于解译秦岭造山带的构造演化过程。以往的研究主要集中在前中生代晚期的剪切变形,而对中生代晚期的剪切变形关注较少。这限制了对青澳拗陷晚中生代构造演化的认识。因此,我们对上丹缝合带中段的沙沟剪切带(SGSZ)进行了详细的野外构造分析和实验室分析。沙沟剪切带发育于八里坪岩浆岩南缘,是一条S-SSW向斜的正弦向斜韧性剪切带,具有从顶部到ESE的剪切意识。岩浆岩原岩为大量晚三叠世花岗岩(200-215Ma)以及少量新近纪花岗岩(759Ma)和早白垩世花岗岩(145Ma)。微观结构和地温仪结果表明,韧性剪切变形发生在地壳中层深度(13-21 千米)的高绿泥石-低闪长岩成因条件下(400-650°C)。锆石U-Pb和闪长岩-生物岩40Ar/39Ar年代测定结果将剪切变形的时间推定为135-145Ma,将SGSZ的快速出露推定为115-135Ma。结合区域数据,我们认为SGSZ的正弦走向剪切变形控制并容纳了东SQB在大陆内部压缩作用下的向东南挤压。随后,大陆内部的延伸导致了SGSZ的快速隆升。
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引用次数: 0
Renewable energy, financial globalization and load capacity factor in the US: Ecological neutrality in the context of natural resources 美国的可再生能源、金融全球化和负载能力系数:自然资源背景下的生态中和
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-08-22 DOI: 10.1002/gj.5043
Saifullahi Sani Ibrahim, Ahmed Samour, Hamza Almassri, Joanna Kurowska‐Pysz
The United States (US) as the second leading economy in global ecological pollution has become a fertile ground for a rigorous analysis of the ecological neutrality using load capacity factor (LCF) and carbon‐based consumption (CCO2). This is important for the global drive of achieving environmental sustainability by 2050. The LCF is one of the most comprehensive ecological proxies that incorporate the biocapacity and ecological footprint. In this context, this research examines the effect of natural resources, technological innovation, renewable energy and financial globalization on ecological neutrality in the US for the date spanning from 1990 to 2021. Using the novel augmented auto‐regressive distributive lag (AARDL) model, the empirical findings of this study indicate that (i) natural resources, renewable energy, and technological innovation promote ecological neutrality by increasing LCF and decreasing CCO2 emissions; (ii) financial globalization and economic growth mitigate the LCF and increase CCO2 emissions; and (iii) a causal effect is observed among technological innovation, natural resources, renewable energy, CCO2 and LCF. In light of the findings, this study recommends several crucial measures for ecological neutrality targets set out in sustainable development goals (SDGs) 7 and 13, respectively.
作为全球生态污染第二大经济体,美国已成为利用负载能力系数(LCF)和碳基消耗(CCO2)对生态中性进行严格分析的沃土。这对于全球推动在 2050 年前实现环境可持续发展非常重要。LCF 是包含生物容量和生态足迹的最全面的生态代用指标之一。在此背景下,本研究探讨了自然资源、技术创新、可再生能源和金融全球化对美国 1990 年至 2021 年生态中和的影响。利用新颖的增强自回归分布滞后(AARDL)模型,本研究的实证结果表明:(i) 自然资源、可再生能源和技术创新通过增加 LCF 和减少 CCO2 排放促进生态中性;(ii) 金融全球化和经济增长缓解 LCF 并增加 CCO2 排放;(iii) 技术创新、自然资源、可再生能源、CCO2 和 LCF 之间存在因果效应。根据研究结果,本研究建议采取几项关键措施,分别实现可持续发展目标(SDGs)7 和 13 中规定的生态中和目标。
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引用次数: 0
Analysis of Carboniferous‐Permian coal‐accumulating environment and coalbed methane enrichment in the southern Qinshui Basin 沁水盆地南部石炭纪-二叠纪煤炭赋存环境及煤层气富集分析
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-08-22 DOI: 10.1002/gj.5050
Xiaojun Zhang
Global research on the geological particularities of coal‐accumulating environments and the enrichment patterns of coalbed methane (CBM) is still relatively weak. This paper studies the geological characteristics and coal accumulation patterns of Carboniferous‐Permian coal‐bearing seams in the southern Qinshui Basin. The results show that the coal‐bearing strata in the basin represent the offshore marine and continental intercalated coal seam sediments developed. The southern part of the basin is dominated by lacustrine facies, and the delta front sub‐facies is locally developed. The characteristics of coal accumulation environment in the southern Qinshui Basin are characterized by basement properties, fault networks and coal‐bearing sedimentary facies, which collectively control the spatial and temporal distribution characteristics of the coal‐rich belt. The differences in coal accumulation environment in the southern basin affect the tectonic evolution, the thickness of the coal seam roof and floor and the hydrogeological conditions of the coal‐rich area, which further control the CBM enrichment in the Taiyuan‐Shanxi Formation. The aim of this study is to explore the factors of CBM enrichment and gas control mode, so as to enrich and improve the theory and method of CBM exploration, which will also help identify the appropriate underground geological structure environment for carbon sequestration (CCS), reduce greenhouse gas emissions and effectively respond to the challenge of global warming.
全球对煤炭赋存环境地质特征和煤层气富集规律的研究还相对薄弱。本文研究了沁水盆地南部石炭系-二叠系含煤地层的地质特征和煤炭赋存规律。结果表明,盆地内的含煤地层为近海海相、大陆相夹层煤层沉积发育。盆地南部以湖相地层为主,局部发育三角洲前缘亚地层。沁水盆地南部煤炭堆积环境的特征主要表现在基底性质、断层网络和含煤沉积面上,它们共同控制了富煤带的时空分布特征。盆地南部煤炭堆积环境的差异影响了富煤区的构造演化、煤层顶底板厚度和水文地质条件,进一步控制了太原-山西地层中煤层气的富集。本研究旨在探讨煤层气富集因素及气体控制模式,以丰富和完善煤层气勘探理论和方法,同时也有助于确定合适的碳封存(CCS)地下地质构造环境,减少温室气体排放,有效应对全球变暖的挑战。
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引用次数: 0
Reliability-based state parameter liquefaction probability prediction using soft computing techniques 利用软计算技术进行基于可靠性的状态参数液化概率预测
IF 1.4 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-08-21 DOI: 10.1002/gj.5049
Kishan Kumar, Pijush Samui, S. S. Choudhary

The state parameter (ѱ) accounts for both relative density and effective stress, which influence the cyclic stress or liquefaction characteristic of the soil significantly. This study presents a ѱ-based probabilistic liquefaction evaluation method using six soft computing (SC) techniques. The liquefaction probability of failure (PL) is calculated using the first-order second moment (FOSM) method based on the cone penetration test (CPT) database. Then, six SC techniques, such as Gaussian process regression (GPR), relevance vector machine (RVM), functional network (FN), genetic programming (GP), minimax probability machine regression (MPMR) and multivariate adaptive regression splines (MARS), are used to predict PL. The performance of these models is examined using nine statistical indices. Additionally, plots such as regression plots, Taylor diagrams, error matrix and rank analysis are shown to assess the SC model's performance. Finally, sensitivity analysis is performed using the cosine amplitude method (CAM) to assess the influence of input parameters on output. The current study demonstrates that SC models based on state parameter predict PL effectively. RVM and MPMR models closely follow the GPR model in terms of performance, which is superior to the other models. Notably, two equations are generated using GP and MARS models to predict PL. The results of the sensitivity analysis reveal the magnitude of earthquake (Mw) as the most sensitive parameter. The outcomes of this research will offer risk evaluations for geotechnical engineering designs and expand the use of state parameter-based SC models in liquefaction analysis.

状态参数(ѱ)考虑了相对密度和有效应力,它们对土壤的循环应力或液化特性有重大影响。本研究利用六种软计算(SC)技术提出了一种基于ѱ 的液化概率评估方法。液化破坏概率(PL)是根据锥入度试验(CPT)数据库,采用一阶第二矩(FOSM)方法计算得出的。然后,使用高斯过程回归 (GPR)、相关性向量机 (RVM)、功能网络 (FN)、遗传编程 (GP)、最小概率机回归 (MPMR) 和多变量自适应回归样条 (MARS) 等六种 SC 技术来预测液化破坏概率。这些模型的性能通过九项统计指标进行检验。此外,还展示了回归图、泰勒图、误差矩阵和等级分析等图表,以评估 SC 模型的性能。最后,使用余弦振幅法(CAM)进行了敏感性分析,以评估输入参数对输出的影响。目前的研究表明,基于状态参数的 SC 模型能有效预测 PL。RVM 和 MPMR 模型的性能紧随 GPR 模型,优于其他模型。值得注意的是,使用 GP 和 MARS 模型生成了两个方程来预测 PL。敏感性分析结果表明,震级(Mw)是最敏感的参数。该研究成果将为岩土工程设计提供风险评估,并扩大基于状态参数的 SC 模型在液化分析中的应用。
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引用次数: 0
Geological characteristics and ore‐forming conditions of the Tasikmadu porphyry Cu–Au prospect in Trenggalek, East Java, Indonesia 印度尼西亚东爪哇 Trenggalek 的 Tasikmadu 斑岩型铜金矿的地质特征和成矿条件
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-08-17 DOI: 10.1002/gj.5042
Arifudin Idrus, Genki Kaneko, Ryohei Takahashi, Finlan Adhitya Aldan, Trifatama Rahmalia, Hinako Sato
Tasikmadu is a newly discovered porphyry Cu–Au prospect in the eastern Sunda arc, Indonesia. This study aimed to elucidate salient diagnostic characteristics and ore‐forming conditions of the prospect. Fieldwork and various laboratory analyses for a suite of representative samples were performed for mineralogy, bulk‐geochemistry, mineral chemistry and ore fluid characterization. The study area is composed of three diorite porphyries, that is, fine‐grained, medium‐grained and coarse‐grained diorite porphyry, respectively. The intrusions are calc‐alkaline with a high Sr/Y value, which is similar to many ore‐bearing intrusions in the eastern Sunda arc. Ore mineralization occurs in quartz veins and veinlet stockwork, centred in the potassic zone, and dominated by chalcopyrite and bornite occurring in A and B veins, which cut earlier barren (EB) and M veins. The mineralization core has an average grade of 0.63 wt% Cu and 0.25 ppm Au, respectively. Outwardly, the potassic zone changes to the propylitic zone, which still bears copper in the quartz and pyrite veinlets, although the grade is low. Fluid inclusion microthermometry revealed that the A and B veins in the potassic zone formed at 464 and 390°C by hypersaline boiling fluids, respectively. The temperature temporally and spatially decreased, that is, in the propylitic zone, the quartz veinlets formed at 260–400°C. Hypogene mineralization that formed the A veins occurred at 1.5 km below the palaeosurface, indicating a relatively shallow depth as a porphyry deposit. Nevertheless, the δ34SCDT values of sulphides range from −2.0 to −0.1‰, inferring a magmatic origin. The Tasikmadu prospect shares some similarities compared with other porphyry deposits worldwide, but it also reveals unique characteristics that differ from others, for example, potassic‐altered rocks are only typified by secondary biotite without/rare secondary K‐feldspar reflecting the lack of magma contamination by continental crustal components. In addition, current surface geological features and shallow depth erosion level of the prospect may imply that the potential of Cu–Au mineralization underneath is still open to depth.
Tasikmadu 是印度尼西亚巽他弧东部新发现的斑岩型铜金矿远景区。这项研究旨在阐明该探矿区的显著诊断特征和成矿条件。对一系列具有代表性的样本进行了矿物学、块状地球化学、矿物化学和矿液特征的实地考察和各种实验室分析。研究区域由三个闪长岩斑岩组成,分别为细粒、中粒和粗粒闪长岩斑岩。侵入体呈钙碱性,锶/钇值较高,与东巽他弧的许多含矿侵入体相似。矿石成矿分布在石英脉和细脉网中,以钾长石带为中心,主要是A脉和B脉中的黄铜矿和辉铜矿,它们切割了早期的贫瘠(EB)脉和M脉。矿化核心的平均品位分别为 0.63 wt% 铜和 0.25 ppm 金。向外,钾长石带转变为丙长石带,虽然品位较低,但石英和黄铁矿细脉中仍含有铜。流体包裹体微测温法显示,钾盐岩带的 A 和 B 矿脉分别是在 464 和 390°C 高温下由超盐沸腾流体形成的。温度在时间和空间上都有所下降,也就是说,在丙铁质区,石英细脉是在 260-400°C 时形成的。形成 A 矿脉的下成矿作用发生在古地表以下 1.5 千米处,这表明斑岩矿床的深度相对较浅。尽管如此,硫化物的 δ34SCDT 值在 -2.0 到 -0.1‰ 之间,推断其来源于岩浆。与世界上其他斑岩矿床相比,Tasikmadu 勘探区有一些相似之处,但也显示出不同于其他矿床的独特特征,例如,钾盐蚀变岩仅以次生生物黄铁矿为典型特征,没有/很少有次生 K 长石,这反映出岩浆没有受到大陆地壳成分的污染。此外,该探矿区目前的地表地质特征和较浅的深度侵蚀程度可能意味着其地下的铜金矿化潜力仍然向深部开放。
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引用次数: 0
The superposition of Cretaceous mineralization events leading to the formation of the large Baiyinnuoer Pb–Zn deposit in NE China 白垩纪成矿事件的叠加导致中国东北白音诺尔大型铅锌矿床的形成
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-08-17 DOI: 10.1002/gj.5039
Ruiliang Wang, Jie Wang, Yuling Zhao, Qingdong Zeng, Xiaowei Wang, Jinzhong Yang, Yunpeng Guo, Bing Yu, Jinjian Wu
The Baiyinnuoer Pb–Zn deposit, estimated at 26.57 million metric tonnes (Mt) with grades of 1.77% Pb and 5.21% Zn, is situated in the southern Great Xing'an Range (SGXR) of northeast China. The deposit comprises southern and northern ore belts. The southern belt primarily contains skarn ore bodies (32% of reserves) associated with Triassic granodiorite, while the northern belt is dominated by skarn ore bodies (30% of reserves) related to Triassic diorite porphyry. In addition to Triassic skarn‐type mineralization, the deposit also exhibits Early Cretaceous mineralization. This includes vein‐type occurrences (36% of reserves) within volcanic tuff and syenite porphyry, alongside a small amount of skarn ore bodies (2% of reserves) related to syenite porphyry. LA‐ICP‐MS U–Pb dating of intrusive rocks and garnets was conducted to investigate the timing and genesis of these mineralization events, revealing two distinct stages of skarn‐type mineralization. The first stage, associated with Early Triassic granitoids, dates to 254.6 ± 1.4–241.7 ± 2.7 Ma, while the second stage is closely associated with Early Cretaceous syenite porphyry, constrained to 135.4 ± 1.1–135.2 ± 1.6 Ma. Garnet U–Pb dating in the syenite porphyry‐related skarn yielded an age of 134.9 ± 4.7 Ma; however, due to low U content, reliable dating of garnets associated with Early Triassic granitoid‐related skarn was not feasible. Micro‐thermometry and Laser Raman analyses of fluid inclusions within vein‐type ore bodies highlighted distinct differences between vein‐type mineralization and Early Triassic skarn‐type mineralization. Additionally, in situ sulfur isotope analyses of sphalerite from both Early Triassic and Early Cretaceous ore bodies indicate a magmatic origin for sulfur in both stages. Through comprehensive geological, geochronological, in situ sulfur isotope and fluid inclusion studies, the Baiyinnuoer Pb–Zn deposit is conclusively identified as a large deposit characterized by two distinct periods of mineralization (Early Triassic and Early Cretaceous), akin to several other significant polymetallic deposits in NE China.
白音诺尔铅锌矿位于中国东北大兴安岭南部,估计储量为 2 657 万吨,铅品位为 1.77%,锌品位为 5.21%。矿床由南部和北部矿带组成。南部矿带主要是与三叠系花岗闪长岩有关的矽卡岩矿体(占储量的 32%),北部矿带主要是与三叠系闪长岩斑岩有关的矽卡岩矿体(占储量的 30%)。除三叠纪矽卡岩型矿化外,该矿床还展示了早白垩世矿化。这包括火山凝灰岩和正长斑岩中的脉型矿点(占储量的 36%),以及与正长斑岩有关的少量矽卡岩矿体(占储量的 2%)。为了研究这些成矿事件的时间和成因,对侵入岩和石榴石进行了 LA-ICP-MS U-Pb 测定,揭示了矽卡岩型成矿的两个不同阶段。第一阶段与早三叠世的花岗岩有关,可追溯到 254.6 ± 1.4-241.7 ± 2.7 Ma,而第二阶段与早白垩世的正长斑岩密切相关,可追溯到 135.4 ± 1.1-135.2 ± 1.6 Ma。正长斑岩相关矽卡岩中的石榴石U-Pb年代测定结果为134.9 ± 4.7 Ma;但是,由于铀含量较低,与早三叠世花岗岩相关矽卡岩有关的石榴石的可靠年代测定并不可行。对矿脉型矿体中的流体包裹体进行的显微测温和激光拉曼分析突出显示了矿脉型矿化与早三叠世矽卡岩型矿化之间的明显差异。此外,对早三叠世和早白垩世矿体中闪锌矿的原位硫同位素分析表明,这两个阶段的硫都来源于岩浆。通过全面的地质、地质年代、原位硫同位素和流体包裹体研究,白音诺尔铅锌矿被确定为一个大型矿床,具有两个不同的成矿期(早三叠世和早白垩世),与中国东北地区其他几个重要的多金属矿床类似。
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引用次数: 0
Design and construction of tunnels and tunnelling: Understanding the importance of geological conditions, landslide susceptibility and risk assessment 隧道和隧道工程的设计与施工:了解地质条件、滑坡易发性和风险评估的重要性
IF 1.4 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-08-14 DOI: 10.1002/gj.5041
Wengang Zhang, Ian Somerville, Gustavo Paneiro, Xingzhong Nong, Marcin Chwala, Wenyu Yang

Tunnel engineering is a complex and multidisciplinary field that requires the integration of geological expertise, advanced modeling techniques, and practical engineering solutions. The research compiled in the Special Issue "Tunnels and Tunneling" makes significant contributions to the field by addressing the diverse geological conditions and intricate challenges inherent in tunnel construction. These insights are crucial for enhancing the safety, efficiency, and sustainability of tunnel projects worldwide. The studies in this Special Issue provide a comprehensive understanding of the various challenges and innovative solutions in tunnel engineering. They offer valuable insights and practical guidelines for designing, constructing, and maintaining safe and stable tunnel structures across different geological settings. In addition, geological challenges in specific regions, such as the Three Gorges Reservoir area, the Hengduan Mountains, and the Tibetan Plateau, require tailored approaches. A key theme in many of the comparative studies is the importance of accurate risk assessment to ensure tunnel safety. In regions prone to geological hazards, landslide susceptibility mapping and risk assessment are critical. Innovative approaches, such as machine learning models, are highlighted for their potential to predict and manage landslide risks effectively.

隧道工程是一个复杂的多学科领域,需要将地质专业知识、先进的建模技术和实用的工程解决方案融为一体。本特刊 "隧道与隧道工程 "中汇集的研究成果针对隧道施工中固有的各种地质条件和复杂挑战,为该领域做出了重大贡献。这些见解对于提高全球隧道项目的安全性、效率和可持续性至关重要。本特刊中的研究全面介绍了隧道工程中的各种挑战和创新解决方案。它们为在不同地质环境下设计、建造和维护安全稳定的隧道结构提供了宝贵的见解和实用指南。此外,特定地区(如三峡库区、横断山脉和青藏高原)的地质挑战也需要量身定制的方法。许多比较研究的一个关键主题是准确的风险评估对确保隧道安全的重要性。在地质灾害频发地区,滑坡易发性测绘和风险评估至关重要。机器学习模型等创新方法因其有效预测和管理滑坡风险的潜力而受到重视。
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引用次数: 0
The effect of soil conditions on the dynamic response of shield tunnels under train-induced vibration loads 土壤条件对列车诱导振动荷载下盾构隧道动态响应的影响
IF 1.4 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-08-14 DOI: 10.1002/gj.5040
Wenbo Yang, Liangliang Zhao, Chaofan Yao, Qixiang Yan, Kun Qian, Jun Yang, Wengang Zhang

In this article, the influence of soil condition on the dynamic response of a tunnel and the surrounding soil was studied by both experimental model tests and numerical simulations. We tested a 1/20-scale tunnel model with three different soil conditions: upper soft soil and lower hard soil, homogeneous soft soil and homogeneous hard soil. We also applied dynamic loads, sweep loads and train loads on the model tunnel for time domain and frequency domain analysis. The experimental and numerical results revealed that the interface between the soft and hard soil strata has an obvious amplification effect on the vibration wave. With the propagation of the vibration wave to the surface, the damping effect of the soil above the tunnel becomes the main factor affecting the dynamic response of soil. The internal force response of the tunnel structure is for the most part concentrated in the section under the excitation load, which is mainly affected by the soil properties beneath the tunnel.

本文通过模型试验和数值模拟两种方法,研究了土壤条件对隧道及其周围土壤动态响应的影响。我们对 1/20 比例的隧道模型进行了三种不同土壤条件的测试:上软下硬、均质软土和均质硬土。我们还对模型隧道施加了动载荷、扫载荷和列车载荷,进行了时域和频域分析。实验和数值结果表明,软硬土层界面对振动波有明显的放大作用。随着振动波向地表传播,隧道上部土体的阻尼效应成为影响土体动力响应的主要因素。隧道结构的内力响应大部分集中在激励荷载作用下的部分,主要受隧道下方土质的影响。
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引用次数: 0
Late Mesoproterozoic passive continental margin in the northwestern Yangtze Block, South China: Insights from the Huodiya Group in the Hannan‐Micangshan Massif 华南扬子地块西北部中新生代晚期被动大陆边缘:汉南米仓山地块霍地牙组的启示
IF 1.8 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-08-13 DOI: 10.1002/gj.5033
Bo Hui, Yunpeng Dong, Shengsi Sun, Feifei Zhang, Xin Zhu, Neda Tavakoli, Yongcheng Li, Rutao Zang
Whether the Yangtze Block was involved in the global late Mesoproterozoic orogeny remains contentious. The Mesoproterozoic Huodiya Group exposed in the Hannan‐Micangshan Massif on the northwestern margin of the Yangtze Block could provide sufficient evidence to further clarify the regional tectonic affinity. However, quantitative insights into the depositional age, provenance and basin tectonic setting of the Huodiya Group still lack comprehensively constraining. This study presents a combined analysis of zircon U–Pb dating for meta‐sedimentary rocks of the Shangliang Formation of the upper Huodiya Group and intruded gabbroic dykes. Intergraded dating results constrain the late Mesoproterozoic maximum depositional age at ca. 1050 Ma. Ca. 900 Ma formation age for the intruded gabbroic dyke, plus the minimum formation age of the overlying Xixiang Group at ca. 950 Ma, further suggests its deposition should be prior to ca. 950–900 Ma. Concordant detrital zircon ages define pronounced age clusters of ca. 2229–1741 and 2950–2388 Ma and few age populations of ca. 3232–3082 and 1069–1033 Ma, consistent with the tectonothermal events in proximal domains at the northwestern and northern Yangtze Block. Detrital zircon age distribution patterns and cumulative curves, coupled with the stable carbonate platform and shallow‐marine facies sedimentation, suggest a passive continental margin setting for the Huodiya Group on the Yangtze Block margin at the late Mesoproterozoic. Comparative insights into the contemporaneous passive continental margin from north to southwest argue against the existence of a late Mesoproterozoic orogeny along the exterior periphery of the Yangtze Block.
长江地块是否参与了全球晚中生代造山运动仍存在争议。出露于扬子地块西北缘汉南米仓山地块的中新生代霍地牙组可为进一步明确区域构造亲缘关系提供充分证据。然而,对霍地牙组的沉积时代、产状和盆地构造背景仍缺乏全面的定量认识。本研究结合锆石U-Pb测年结果,对霍地牙上组上梁层的元沉积岩和侵入辉长岩岩体进行了分析。综合测年结果将中新生代晚期的最大沉积年龄推定为约1050Ma。1050 Ma。侵入岩的形成年龄约为 900 Ma。侵入辉长岩堤的形成年龄约为 900 Ma,加上上覆西乡组的最小形成年龄约为 950 Ma,进一步表明其沉积年龄约为 1050 Ma。950 Ma,进一步表明其沉积时间应早于约 950-900 Ma。一致的碎屑锆石年龄确定了约 2229-1741 Ma 和 2950-2388 Ma 的明显年龄群,以及约 3232-3082 Ma 和 1069-1033 Ma 的少数年龄群,与西北部和北部扬子地块近域的构造热事件相一致。碎屑锆石年龄分布模式和累积曲线,以及稳定的碳酸盐岩平台和浅海面沉积,表明霍地牙组在中新生代晚期处于长江地块边缘的被动大陆边缘环境。从北部到西南部对同时代被动大陆边缘的比较研究表明,长江地块外围并不存在中新生代晚期的造山运动。
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引用次数: 0
Case study of a cluster of simple and complex monogenetic volcanoes in the north-east part of the Michoacan–Guanajuato Volcanic Field, Central Mexico: Nomenclature implications 墨西哥中部米却肯-瓜纳华托火山区东北部简单和复杂单源火山群案例研究:命名的影响
IF 1.4 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-08-13 DOI: 10.1002/gj.5025
Pooja Kshirsagar, Raúl Miranda Aviles, María Jésus de Puy y Alquiza, Boris Chako Tchamabe, Andrés Josué Campos Dominguez

With the advent of new terminologies to categorize and characterize the simple and complex monogenetic volcanoes, also came the semantic issues, which caused a predicament for the usage of terms like simple, complex, polycyclic, polymagmatic, complex monogenetic volcanoes with polygenetic inheritance. To analyse and validate this nomenclature, we studied an overlapping volcanic structure located south of the present-day town of Irapuato, Central Mexico, that appears to be a monogenetic complex at first sight. Field observations, tephra stratigraphy, petrography and geochemistry of the tephra deposits confirms that the structure is in fact a cluster of three simple (San Joaquin tuff ring and two scoria mounds) and one complex, polycyclic, polymagmatic (La Sanabria-San Roque tuff ring) monogenetic volcanoes formed by independent events, governed by distinct conduits and magma bodies of different origin (subduction-related, OIB and E-MORB origin) and separated by different tephra sequences of dissimilar components and depositional characteristics. We estimate the magma volumes (using the juvenile content and their vesicularity percentage) to be at 0.40–1.31 × 108, 0.25 × 108 and 0.42–0.90 × 108 m3 for San Joaquin, La Sanabria and San Roque, reckoning an eruption duration of 77 and 48 and 81 days, respectively (considering an average eruption rate of 6 m3/s from the well-documented shallow crater (<30 m), Ukinrek maars in Alaska) occurring within the age range of 40–70 k years (crater diameter and depth ratio). This study not only aided to validate the above-mentioned terms for monogenetic volcanoes, but also reconsider a few of them and avoid confusion with the polygenetic counterparts.

随着用于分类和描述简单和复杂单源火山的新术语的出现,语义问题也随之而来,这给使用简单、复杂、多环、多形态、多基因遗传的复杂单源火山等术语造成了困境。为了分析和验证这些术语,我们研究了位于现今墨西哥中部伊拉普阿图镇南部的一个重叠火山结构,乍一看,它似乎是一个单源复合火山。实地观察、表土沉积的地层学、岩石学和地球化学证实,该结构实际上是由三个简单的(圣华金凝灰岩环和两个灼烧岩丘)和一个复杂的、多环的火山群组成、这些火山由不同的导管和不同来源(俯冲相关、OIB 和 E-MORB)的岩浆体所控制,并被不同成分和沉积特征的不同表灰岩序列所分隔。我们估算的岩浆体积(使用幼体含量及其泡状百分比)分别为 0.40-1.31 × 108、0.25 × 108 和 0.42-0.90 × 108 立方米。圣华金火山、拉萨纳布里亚火山和圣洛克火山的岩浆量分别为 0.40-1.31 × 108、0.25 × 108 和 0.42-0.90 × 108 立方米,喷发持续时间分别为 77 天、48 天和 81 天(考虑到阿拉斯加乌金雷克火山口(30 米)的平均喷发速度为 6 立方米/秒),喷发年龄范围为 40-70 千年(火山口直径和深度比)。这项研究不仅有助于验证上述有关单基因火山的术语,还重新考虑了其中一些术语,避免了与多基因火山相混淆。
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引用次数: 0
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Geological Journal
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