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Probing environmental sustainability aspects of resource efficiency, renewable energy usage and globalization 探索环境可持续性方面的资源效率,可再生能源的使用和全球化
IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-11-26 DOI: 10.1016/j.gr.2024.10.016
Oktay Özkan , Hephzibah Onyeje Obekpa , Stephen Taiwo Onifade , Andrew Adewale Alola
Given the pace of economic expansion arising from energy usage among other social and economic factors, emerging economies such as Turkey are increasingly becoming the focus for a net zero future. Therefore, the current attempt considers the drivers of environmental sustainability via load capacity factor (LCF) in the context of resource efficiency, renewable energy utilization, and globalization for Turkey over the period 1982 to 2019. By employing series of empirical tools that include cross-quantilogram method, quantile-on-quantile regression, quantile regression approaches, and the nonparametric quantile Granger causality approach, the result shows there is statistically significant evidence of quantile-to-quantile dependence among the trio of (resource efficiency, renewable energy utilization, and globalization) and LCF such that the dependence it reflects some levels of positive directional predictability, thus showing that these indicators are important drivers of environmental sustainability in Turkey. Furthermore, for the quantile-on-quantile regression results, there are statistically significant and positive effects of (i) resource efficiency on LCF across its conditional quantiles of distribution, (ii) renewable energy utilization on LCF and is mostly visible at the lower quantile up to the upper middle quantiles of renewable energy utilization (0.05–0.65), and (iii) globalization on LCF across the lower to upper middle quantiles. With the other empirical approaches providing similar results, the outcome of this investigation offers specific policy insight into resource circularity and energy efficiency.
鉴于能源使用以及其他社会和经济因素带来的经济扩张速度,土耳其等新兴经济体正日益成为未来净零排放的焦点。因此,目前的尝试考虑了1982年至2019年期间土耳其在资源效率、可再生能源利用和全球化背景下,通过负荷能力因子(LCF)来实现环境可持续性的驱动因素。通过交叉量化图方法、分位数对分位数回归、分位数回归方法和非参数分位数格兰杰因果关系方法等一系列实证工具,结果表明,资源效率、可再生能源利用和全球化三者与LCF之间存在显著的分位数对分位数相关性,这种相关性在一定程度上反映了正向的可预测性。从而表明这些指标是土耳其环境可持续性的重要驱动因素。此外,对于分位数对分位数的回归结果,(i)资源效率对LCF的影响在其条件分布分位数上具有统计学意义和积极的影响,(ii)可再生能源利用对LCF的影响在可再生能源利用的下至中上分位数(0.05-0.65),以及(iii)全球化对LCF的影响在中下至中上分位数上最为明显。由于其他实证方法提供了类似的结果,本调查的结果为资源循环和能源效率提供了具体的政策见解。
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引用次数: 0
Glacial fluctuations in the Cryogenian Marinoan Snowball Earth 冰冻期Marinoan雪球地球的冰川波动
IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-11-22 DOI: 10.1016/j.gr.2024.10.015
Gang Wang , Kun Zhao , Jingxuan Zhang , Shengxian Zhu , Chaochao Xing , Xianguo Lang
The Marinoan glaciation represents the pinnacle of glacial severity in Earth’s geological history. Deep-water glacial deposits have revealed a complex interplay of at least two glacial advance-retreat cycles. However, the extent to which these glacial episodes are mirrored in shallow-water settings has received less attention. To shed light on this, we undertook an exhaustive lithofacies analysis of three shallow-water sections within the Nantuo Formation in South China. Our findings delineate six distinct lithofacies within the Nantuo Formation: massive diamictite, crudely stratified diamictite, pebbly sandstone, massive sandstone, dropstone-bearing laminated siltstone/mudstone, and laminated mudstone/siltstone. The vertical successions of these lithofacies have allowed us to identify two facies associations indicative of glacial dynamics; they are the ice-grounding line fan facies association and the ice-distal facies association. By juxtaposing our findings with the facies analysis of three deep-water sections, we have established a lateral correlation, confirming the presence of at least two glacial advance and retreat cycles in shallow-water environments. Each glacial advance is marked by the presence of inversely graded massive diamictite, indicative of ice-proximal, glaciomarine conditions. In contrast, each retreat phase is characterized by a fining-upward sequence from siltstone to mudstone, interspersed with dropstones, signifying ice-distal, glaciomarine settings. This study not only underscores the dynamic character of the Marinoan snowball Earth glaciation but also suggests that the glacial oscillations observed in deep-water environments have counterparts in shallow waters. It provides evidence that the scale of the Marinoan glacial fluctuations was not confined to the deep ocean but extended to encompass the entire basin, offering a more comprehensive understanding of the Earth’s climatic and glacial history during this critical period.
马里诺冰期代表了地球地质史上冰川严重程度的顶峰。深水冰川沉积物揭示了至少两个冰川进退旋回的复杂相互作用。然而,这些冰川时期在浅水环境中反映的程度受到的关注较少。为了阐明这一点,我们对中国南方南沱组三个浅水剖面进行了详尽的岩相分析。研究结果将南沱组划分为块状二晶岩、粗层状二晶岩、含砾砂岩、块状砂岩、含浮石层状粉砂岩/泥岩、层状泥岩/粉砂岩6种不同的岩相。这些岩相的垂向序列使我们能够确定两种指示冰川动力学的相组合;它们分别是冰-接地线扇相组合和冰-远端相组合。通过将我们的发现与三个深水剖面的相分析并置,我们建立了横向相关性,证实了在浅水环境中至少存在两次冰川进退旋回。每次冰期推进的标志都是出现了反序级的块状杂晶岩,表明冰近端冰期海洋条件。相比之下,每个后退阶段的特征是一个从粉砂岩到泥岩的细化向上序列,点缀着落石,表明冰远端,冰川海洋环境。该研究不仅强调了马里诺雪球地球冰川的动力学特征,而且表明在深水环境中观测到的冰川振荡在浅水环境中也有对应。它提供的证据表明,马里诺冰期波动的规模并不局限于深海,而是扩展到整个盆地,从而使人们对这一关键时期的地球气候和冰川历史有了更全面的了解。
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引用次数: 0
New Swartpuntia occurrence found within the Aar Member 在阿尔(Aar)岩层中发现新的 Swartpuntia 分布区
IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-11-14 DOI: 10.1016/j.gr.2024.11.002
Brandt M. Gibson , Ingrid Stengel , Zakeus Nghishidulu , Peter R. Liberty , Ajani Bissick , Andrea Boscaini , Joshua H.F.L. Davies , Galen P. Halverson , Frederick J. Hilgen , Bianca Spiering , Patricia Vickers-Rich , Marc Laflamme
A new occurrence of Swartpuntia germsi is reported from Farm Aar near Aus in southern Namibia. It is preserved as incomplete part/counterpart in two dimensions, with a folded petaloid. Stratigraphically correlated to a minimum depositional age of 547.32 ± 0.31 Ma, this represents the oldest global occurrence of Swartpuntia and documents a unique style of preservation within the Nama Group. Lastly, the occurrence increases the taxonomic and ecological diversity preserved at Farm Aar, making Farm Aar one of the only locations to preserve all common forms of Erniettomorph taxa.
据报道,纳米比亚南部奥斯附近的阿尔农场新发现了一种 Swartpuntia germsi。它以不完整的部分/对应部分的形式保存在二维空间中,并带有一个折叠的花瓣。从地层学角度看,其最小沉积年龄为 547.32 ± 0.31 Ma,这是全球发现的最古老的疣螈,并记录了纳马群中一种独特的保存方式。最后,这一发现增加了阿尔农场保存的分类学和生态学多样性,使阿尔农场成为保存所有常见Erniettomorph分类群的唯一地点之一。
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引用次数: 0
Constraining the extent of Greater India: New late Paleocene paleomagnetic data from the Tethyan Himalaya, Tibetan Plateau 制约大印度的范围:来自青藏高原哲罗喜马拉雅山脉的新的古新世晚期古地磁数据
IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-11-14 DOI: 10.1016/j.gr.2024.11.004
Yong Cao , Zhiming Sun , Zhenyu Yang , Haibing Li , Junling Pei , Xiaozhou Ye , Xinwen Cao , Bailing Wu , Chenguang Liu , Lei Zhang
The collision of India and Asia formed the Himalayas and caused the uplift of the Tibetan Plateau. Greater India comprises the part of the Indian plate that was subducted beneath Asia and the Tethyan Himalaya. Quantitative constraints on the extent of Greater India are needed to study the process of the India-Asia collision. However, such constraints are lacking and the topic remains debated. We present paleomagnetic data from late Paleocene (∼58 Ma) mafic rocks from the western Tethyan Himalaya. The mean paleomagnetic direction is Ds/Is = 348.5°/+6.5° with k = 38.7 and a95 = 5.2°, which passed the fold, reversals, and paleosecular variation tests. The results define the paleolatitude of the Tethyan Himalaya as 3.3 ± 4.5°N at ∼ 58 Ma for the reference site of 29.9°N/83.3°E. A comparison of the Paleogene paleolatitudes of the Tethyan Himalaya shows that the terrane moved northward by 1540 ± 290 km between ∼ 60 Ma and ∼ 50 Ma, with a rate of movement of 15.4 ± 2 cm/yr. The new paleomagnetic result confirms that the extent of Greater India was 1130 ± 400 km and was essentially uniform from east to west. This finding implies that the collision between India and Asia was nearly be quasi-synchronous from the middle-eastern to western segments along the Indus-Tsangpo suture zone.
印度和亚洲的碰撞形成了喜马拉雅山脉,并造成了青藏高原的隆起。大印度板块包括俯冲到亚洲和四叠纪喜马拉雅山之下的印度板块部分。研究印度-亚洲碰撞过程需要对大印度地区的范围进行定量限制。然而,目前还缺乏这样的约束条件,对这一问题仍存在争议。我们展示了来自泰西喜马拉雅西部晚古新世(∼58 Ma)岩浆岩的古地磁数据。平均古地磁方向为Ds/Is = 348.5°/+6.5°,k = 38.7,a95 = 5.2°,通过了褶皱、逆转和古地理变异检验。结果确定了以 29.9°N/83.3°E 为参照地点的哲罗喜马拉雅古纬度为 3.3 ± 4.5°N,时间为 ∼ 58 Ma。通过对比古近纪泰西喜马拉雅山的古纬度,发现该地层在60Ma∼50Ma之间向北移动了1540±290千米,移动速度为15.4±2厘米/年。新的古地磁结果证实,大印度的范围为 1130 ± 400 千米,从东到西基本一致。这一发现意味着印度和亚洲之间的碰撞从印度河-赞普河缝合带的中东部到西部几乎是近乎同步的。
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引用次数: 0
Early Devonian stylonurine eurypterids from northern Gondwana: Late Lochkovian to early Pragian records from South China 来自冈瓦纳北部的早泥盆世stylonurine极龙类:来自华南的晚洛克维期至早期普拉格期记录
IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-11-14 DOI: 10.1016/j.gr.2024.11.003
Zhiheng Ma , James C. Lamsdell , Maxwell Wang , Jingwen Chen , Paul A. Selden , Ben He
This paper describes a new stylonurine eurypterid: Qujingopterus spineus gen. et sp. nov., from the Early Devonian (late Lochkovian to early Pragian) Xitun formation of Yunnan Province, South China. This discovery represents one of the earliest stylonurine records from Gondwana and further supports the global distribution of stylonurines. Considering the probable region of origin of the clade and and their lack of anatomical structures adapted for swimming, we propose that stylonurines migrated to Gondwana as the Rheic Ocean dwindled while Gondwana rapidly approached Laurussia. An additional specimen from this locality is described, and can be assigned to the eurypterine family Pterygotidae. Based on the environmental analysis, it can be inferred that the eurypterids from South China underwent adaptations to cope with decreasing salinity levels. This discovery provides valuable insights into the timing and mechanisms underlying eurypterid invasion into freshwater ecosystems.
本文描述了中国云南西屯早泥盆世(晚泥盆世至早泥盆世)地层中发现的一种新的stylonurine eurypterid:Qujingopterus spineus gen. et sp.这一发现代表了冈瓦纳最早的石龙子记录之一,进一步证实了石龙子的全球分布。考虑到该支系可能的起源地区,以及它们缺乏适应游泳的解剖结构,我们认为,当冈瓦纳迅速接近劳鲁西亚时,莱茵洋逐渐缩小,斯泰隆人迁移到了冈瓦纳。我们还描述了该地点的另一个标本,该标本可归属于翼龙科(Pterygotidae)。根据环境分析,可以推断华南地区的极龙类经历了适应盐度下降的过程。这一发现为了解极翅目昆虫入侵淡水生态系统的时间和机制提供了宝贵的信息。
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引用次数: 0
Scrutinizing the load capacity curve for a global perspective: The role of Fintech, government effectiveness and renewable energy 从全球视角审视负载能力曲线:金融科技、政府效率和可再生能源的作用
IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-11-08 DOI: 10.1016/j.gr.2024.10.014
Ugur Korkut Pata , Kamel Si Mohammed , Cheloufi Omeyr , Selin Karlilar Pata , Hind Alofaysan , Mustafa Tevfik Kartal
With the evolving world order, countries are using financial technologies (Fintech) to access financial resources more effectively, and Fintech can have an impact on the environment. This study aims to investigate the influence of Fintech on ecological sustainability, focusing on the contribution of renewable energy (RE) and government effectiveness (GE) under the Load Capacity Curve (LCC). This research analyzes data from 69 middle-income economies between 2006 and 2022 using the dynamic panel threshold model (DPTR). The outcomes document that GDP reduces the LCF below a certain threshold, but a positive impact above this threshold. Specifically, the model yielded a threshold value of $US 5222.234, which is higher than the average GDP of $US 4276.802. This finding suggests a U-shaped relationship between GDP and LCF, which supports the LCC hypothesis. The outcome also reports that Fintech plays a crucial role in improving ecological sustainability, while government effectiveness has a negative effect. The study emphasizes that middle-income countries should support Fintech and renewable energy along development with economic progress to improve ecological quality.
随着世界秩序的不断发展,各国正在利用金融技术(Fintech)更有效地获取金融资源,而金融技术可能会对环境产生影响。本研究旨在探究金融科技对生态可持续性的影响,重点关注负载能力曲线(LCC)下可再生能源(RE)和政府效能(GE)的贡献。本研究使用动态面板阈值模型(DPTR)分析了 2006 年至 2022 年间 69 个中等收入经济体的数据。研究结果表明,GDP 在低于某一阈值时会降低 LCF,但在该阈值之上则会产生积极影响。具体而言,该模型得出的阈值为 5222.234 美元,高于 4276.802 美元的平均 GDP。研究结果还指出,金融科技在改善生态可持续性方面发挥了关键作用,而政府效能则产生了负面影响。研究强调,中等收入国家在发展经济的同时,应支持金融科技和可再生能源,以改善生态质量。
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引用次数: 0
Contrasting physical erosion rates in cratonic catchments: The Ogooué and Mbei rivers, Western Central Africa 板块集水区截然不同的物理侵蚀率:中非西部的奥戈韦河和姆贝河
IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-11-08 DOI: 10.1016/j.gr.2024.10.013
V. Regard , S. Carretier , J.-S. Moquet , S. Choy , P.-H. Blard , S. Bogning , A.P. Mbonda , E. Mambela , M.C. Paiz , M. Séranne , J. Charreau , D. Rouby , J. Bouchez , J. Gaillardet , J.-J. Braun , Y. Denèle
We measured the long-term physical denudation of the Ogooué River catchment using 10Be produced in situ by cosmic rays. These measurements are averaged over 25–200 ka (average 40 ka), depending on the physical denudation rate. The denudation rate of the Ogooué River catchment is slow (38 t/km2/a, 15 m/Ma), slightly higher than in Equatorial West Africa (from Senegal to Angola, 26 t/km2/a, 10 m/Ma). Physical denudation and chemical weathering fall within the same order of magnitude. Thus, although low, there is substantial chemical weathering compared to physical denudation, that likely contributes over 30 % of the total denudation.
Denudation rates are spatially variable (from 10 to 60 t/km2/a) within the large Ogooué River catchment. Over the long term, physical denudation and chemical weathering roughly match, except in the Batéké Plateaux area, because the plateaus are made up of already weathered detrital material and therefore their modern flux of solutes is very low (∼9.5 t/km2/a). The spatial distribution is similar to the one described in the work of Moquet et al. (2021) on the basis of solute fluxes, i.e. the southern part of the catchment is denuding twice as fast as the northern part. We show here that the whole picture did not vary much since 100 ka, as shown by both methods which give consistent results. Faster denudation in the southern part of the catchment may be related to more uplift than in the northern part caused by the southern African “superswell”.
我们利用宇宙射线在原地产生的 10Be 测量了奥戈韦河流域的长期物理剥蚀情况。根据物理剥蚀速率,这些测量结果的平均值为 25-200 ka(平均 40 ka)。奥戈韦河集水区的剥蚀速率较慢(38 吨/平方公里/年,15 米/兆帕),略高于西非赤道地区(从塞内加尔到安哥拉,26 吨/平方公里/年,10 米/兆帕)。物理剥蚀和化学风化的数量级相同。因此,与物理剥蚀相比,化学风化虽然程度较低,但却占到了剥蚀总量的 30%以上。在奥戈韦河的大集水区内,剥蚀率在空间上存在差异(从 10 吨/平方公里到 60 吨/平方公里不等)。从长期来看,物理剥蚀和化学风化基本一致,但巴特克高原地区除外,因为该地区的高原由已经风化的碎屑物质构成,因此其现代溶质通量非常低(9.5 吨/平方公里/年)。其空间分布与 Moquet 等人(2021 年)根据溶质通量所描述的情况类似,即集水区南部的剥蚀速度是北部的两倍。我们在此表明,两种方法得出的结果一致,自 100 ka 年以来,整个情况变化不大。集水区南部更快的剥蚀可能与南部非洲 "超级海啸 "造成的隆起比北部更多有关。
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引用次数: 0
Crustal thickening, exhumation and metamorphic cooling of Neoproterozoic eclogites in NE Brazil: Timescale for the assembly of West Gondwana 巴西东北部新元古代蚀变岩的地壳增厚、剥蚀和变质冷却:西冈瓦纳组装的时间尺度
IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-11-07 DOI: 10.1016/j.gr.2024.11.001
Alanielson Ferreira , Gary Stevens , Elton L. Dantas , Reinhardt A. Fuck , Ticiano J.S. dos Santos
The high-pressure followed by high-temperature metamorphism related to the evolution of collisional orogens is the expected Pressure-Temperature-time (P-T-t) path for modern-style plate tectonics. However, these P-T-t paths are rarely preserved even in Phanerozoic orogens. In this matter, the Campo Grande migmatite-gneiss area presents an exhumed Archean crust with heterogeneous retrograde eclogites overprinted by amphibolite-facies in NE Brazil. Retrogressed eclogites in the area core are formed by Mn-rich garnet + clinopyroxene porphyroblasts layer with a minor amphibole + quartz + titanite assemblage, whereas the margins display dismembered lenses of Mg-rich garnet porphyroblasts with plagioclase + amphibole coronae and clinopyroxene + plagioclase + ortopyroxene sympleticte mainly within shear zones. Phase equilibria modelling reveals that these distinct retro-eclogites record similar eclogite conditions (up to 18 kbar and 660 ± 20 °C). Mn-rich eclogites display widespread magmatic zoned zircon grains from Mesoarchean to Paleoproterozoic and recrystallized metamorphic grains of 607.7 ± 5.4 Ma. Zircon from Mg-rich eclogites crystallized at 2.67 Ga and overgrowth rims formed at 2.0 Ga and 590.1 ± 1.8 Ma. REE in zircon lack Eu anomaly, displaying flat HREE patterns in 590.1 ± 1.8 Ma Neoproterozoic grains indicate recrystallization under eclogite-facies conditions. In situ U-Pb titanite dating yielded two younger age sets at 574.7 ± 0.5 and 562.8 ± 2.1 Ma. Lastly, in situ U-Pb dating of rutile inclusions in garnet cores present ages of 606.1 ± 4.0 Ma, whereas rutile included in retrograde coronae and sympleticte yielded concordant ages from 559.0 ± 2.3 to 523.2 ± 1.9 Ma. Thus, combined phase equilibria modelling and U-Pb ages reveal a progressive change in metamorphic conditions from eclogite conditions (at least 607.7 ± 5.4 to 590 ± 1.8 Ma; zircon dating and rutile ages included in eclogite garnet) to nearly isothermal decompression (574.7 ± 0.5 Ma; titanite age) of ancient Archean deep crust, which was followed by suggested final exhumation and metamorphic cooling at shallower crustal levels between 559.0 ± 2.3 and 523.2 ± 1.9 Ma (rutile age in retrogressed assemblage). Therefore, the high-pressure conditions followed by decompression and metamorphic cooling during sin- to post-collisional settings were associated with the final assembly of West Gondwana.
与碰撞造山运动演化有关的先高压后高温的变质作用是现代板块构造的预期压力-温度-时间(P-T-t)路径。然而,即使在新生代造山运动中也很少保留这些 P-T-t 路径。在这一问题上,巴西东北部的坎普格兰德伟晶岩-片麻岩地区展示了一个被阿新世地壳挤压的地壳,其上覆盖着闪长岩岩相的异质逆冲闪长岩。该地区核心的逆冲闪长岩由富锰石榴石+霞石斑岩层与少量闪石+石英+榍石组合形成,而边缘则主要在剪切带内显示富镁石榴石斑岩与斜长石+闪石冠层和霞石+斜长石+正长石共生的肢解透镜体。相平衡模型显示,这些不同的后斜长岩记录了相似的蚀变条件(高达 18 千巴和 660 ± 20 °C)。富锰斜长岩显示了从中生代到古近代的广泛岩浆带状锆石颗粒,以及 607.7 ± 5.4 Ma 的重结晶变质岩颗粒。富镁蚀变岩中的锆石在 2.67 Ga 时结晶,在 2.0 Ga 和 590.1 ± 1.8 Ma 时形成过生缘。锆石中的 REE 缺乏 Eu 异常,在 590.1 ± 1.8 Ma 新元古代的晶粒中显示扁平的 HREE 模式,表明是在埃克洛辉石时代的条件下重结晶的。原位铀-铅榍石年代测定得出了两个较年轻的年龄组,分别为 574.7 ± 0.5 Ma 和 562.8 ± 2.1 Ma。最后,对石榴石岩芯中的金红石包裹体进行原位 U-Pb 测定,得出的年龄为 606.1 ± 4.0 Ma,而逆行冠岩和共生岩中的金红石则得出了 559.0 ± 2.3 至 523.2 ± 1.9 Ma 的一致年龄。因此,结合相平衡模型和 U-Pb 年龄可以看出,变质条件从斜长岩条件(至少 607.7 ± 5.4 至 590 ± 1.8 Ma;锆石测年和斜长岩石榴石中的金红石年龄)逐步变化到近乎等温减压条件(574.7 ± 0.5 Ma;钛铁矿测年和金红石年龄)。其后,在 559.0 ± 2.3 至 523.2 ± 1.9 Ma 之间的较浅地壳水平上发生了最后的掘起和变质冷却(逆冲组中的金红石年龄)。因此,在撞击前至撞击后的高压条件下,减压和变质冷却与西冈瓦纳的最终组装有关。
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引用次数: 0
Editorial Board (IFC) 编辑委员会(国际金融公司)
IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-11-05 DOI: 10.1016/S1342-937X(24)00295-8
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引用次数: 0
Enhanced landslide susceptibility mapping in data-scarce regions via unsupervised few-shot learning 在数据稀缺地区,通过无监督的 "少量镜头学习 "增强滑坡易感性绘图
IF 7.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-11-04 DOI: 10.1016/j.gr.2024.10.011
Linghao Kong , Wenkai Feng , Xiaoyu Yi , Zhenghai Xue , Luyao Bai
Given the critical need to assess landslide hazards, producing landslide susceptibility map (LSM) in regions with scarce historical landslide inventories poses significant challenges. This study introduces a novel landslide susceptibility assessment framework that combines unsupervised learning strategies with few-shot learning methods to increase the accuracy of LSM in these areas. The framework has been practically validated in a representative geological disaster-prone area along the West-East Gas Pipeline in Shaanxi Province, China. We employed three advanced few-shot learning models: a support vector machine, meta-learning, and transfer learning. These models implement feature representation learning for weakly correlated influencing factors through an unsupervised approach, thereby constructing an effective landslide susceptibility assessment model. We compared traditional learning methods and used the receiver operating characteristic (ROC) curve and SHAP values to quantify the effectiveness of the models. The results indicate that the meta-learning algorithm outperforms both the SVM and transfer learning in areas with limited landslide data. The integration of unsupervised strategies significantly improves performance, achieving area under the curve (AUC) values of 0.9385 and 0.9861, respectively. Compared with using meta-learning alone, incorporating unsupervised learning strategies increased the AUC by 4.76%, enhancing both the predictive power of the model and the interpretability of the features. Meta-learning under unsupervised conditions effectively mitigates the evaluation difficulties caused by insufficient landslide records, providing a viable path and empirical evidence for performance improvement in similar data- scarce regions worldwide.
鉴于评估滑坡危害的迫切需要,在缺乏历史滑坡资料的地区绘制滑坡易感性地图(LSM)是一项重大挑战。本研究介绍了一种新型滑坡易发性评估框架,该框架将无监督学习策略与少量学习方法相结合,以提高这些地区滑坡易发性地图的准确性。该框架在中国陕西省西气东输管道沿线具有代表性的地质灾害易发区进行了实际验证。我们采用了三种先进的少拍学习模型:支持向量机、元学习和迁移学习。这些模型通过无监督方法对弱相关影响因素进行特征表示学习,从而构建了有效的滑坡易损性评估模型。我们比较了传统的学习方法,并使用接收者操作特征曲线(ROC)和 SHAP 值来量化模型的有效性。结果表明,在滑坡数据有限的地区,元学习算法优于 SVM 和迁移学习。无监督策略的集成显著提高了性能,曲线下面积(AUC)值分别达到 0.9385 和 0.9861。与单独使用元学习相比,整合非监督学习策略后的 AUC 提高了 4.76%,既增强了模型的预测能力,又提高了特征的可解释性。无监督条件下的元学习有效缓解了滑坡记录不足造成的评估困难,为全球类似数据匮乏地区的性能提升提供了可行路径和实证依据。
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Gondwana Research
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