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Multiple Uplift and Exhumation of the Southeastern Tibetan Plateau:Evidence from Low-Temperature Thermochronology 被引量:1
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作者 WU Limin PENG Touping +6 位作者 FAN Weiming ZHAO Guochun GAO Jianfeng DONG Xiaohan PENG Shili MIN Kang Tin Aung MYINT 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2024年第3期569-584,共16页
Since the Cenozoic,the Tibetan Plateau has experienced large-scale uplift and outgrowth due to the India-Asia collision.However,the mechanism and timing of these tectonic processes still remain debated.Here,using apat... Since the Cenozoic,the Tibetan Plateau has experienced large-scale uplift and outgrowth due to the India-Asia collision.However,the mechanism and timing of these tectonic processes still remain debated.Here,using apatite fission track dating and inverse thermal modeling,we explore the mechanism of different phases of rapid cooling for different batholiths and intrusions in the southeastern Tibetan Plateau.In contrast to previous views,we find that the coeval granitic batholith exposed in the same tectonic zone experienced differential fast uplift in different sites,indicating that the present Tibetan Plateau was the result of differential uplift rather than the entire lithosphere uplift related to lithospheric collapse during Cenozoic times.In addition,we also suggest that the 5-2 Ma mantle-related magmatism should be regarded as the critical trigger for the widely coeval cooling event in the southeastern Tibetan Plateau,because it led to the increase in atmospheric CO_(2)level and a hotter upper crust than before,which are efficient for suddenly fast rock weathering and erosion.Finally,we propose that the current landform of the southeastern Tibetan Plateau was the combined influences of tectonic and climate. 展开更多
关键词 apatite fission track rapid cooling differential uplift MAGMATISM southeastern Tibetan Plateau
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Hydrocarbon Generation Potential and Organic Matter Enrichment Mechanism of the Cambrian Marine Shale in the Tadong Low Uplift,Tarim Basin
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作者 MIAO Huan WANG Yanbin +5 位作者 JIANG Zhenxue ZHAO Shihu SHANG Peng GONG Xun TAO Chuanqi ZHANG Yu 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2024年第5期1301-1321,共21页
Cambrian shales in China and elsewhere contain abundant oil and gas resources.However,due to its deep burial and limited outcrop,there has been relatively little research conducted on it.The Cambrian shale of the Tado... Cambrian shales in China and elsewhere contain abundant oil and gas resources.However,due to its deep burial and limited outcrop,there has been relatively little research conducted on it.The Cambrian shale of the Tadong low uplift in the Tarim Basin of western China,specifically the Xidashan-Xishanbulake Formation(Fm.)and overlying Moheershan Fm.provide a case study through the use of organic petrology,mineralogy,organic and elemental geochemistry,with the aim of analyzing and exploring the hydrocarbon generation potential(PG)and organic matter(OM)enrichment mechanisms within these shale formations.The results indicate that:(1)the Cambrian shale of the Tadong low uplift exhibits relatively dispersed OM that consists of vitrinite-like macerals and solid bitumen.These formations have a higher content of quartz and are primarily composed of silica-based lithology;(2)shale samples from the Xidashan-Xishanbulake and Moheershan formations demonstrate high total organic carbon(TOC)and low pyrolytic hydrocarbon content(S_(2))content.The OM is predominantly typeⅠand typeⅡkerogens,indicating a high level of maturation in the wet gas period.These shales have undergone extensive hydrocarbon generation,showing characteristics of relatively poor PG;(3)the sedimentary environments of the Xidashan-Xishanbulake and Moheershan formations in the Tadong low uplift are similar.They were deposited in warm and humid climatic conditions,in oxygen-deficient environments,with stable terrigenous inputs,high paleoproductivity,high paleosalinity,weak water-holding capacity,and no significant hydrothermal activity;and(4)the relationship between TOC and the paleoproductivity parameter(P/Ti)is most significant in the Lower Cambrian Xidashan-Xishanbulake Fm.,whereas correlation with other indicators is not evident.This suggests a productivity-driven OM enrichment model,where input of landderived material was relatively small during the Middle Cambrian,and the ancient water exhibited lower salinity.A comprehensive pattern was formed under the combined control of paleoproductivity and preservation conditions.This study provides valuable guidance for oil and gas exploration in the Tarim Basin. 展开更多
关键词 Conventional resources hydrocarbon generation potential geochemistry sedimentary environment enrichment mechanism organic matter CAMBRIAN Tadong low uplift
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An improved analytical solution for solving the shield tunnel uplift problem
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作者 Bin Wang Jietao Li +1 位作者 Chenyang Zhao Jun Wang 《Journal of Rock Mechanics and Geotechnical Engineering》 SCIE CSCD 2024年第11期4570-4585,共16页
The problem of shield tunnel uplift is a common issue in tunnel construction.Due to the decrease in shear stiffness at the joints between the rings,uplift is typically observed as bending and dislocation deformation a... The problem of shield tunnel uplift is a common issue in tunnel construction.Due to the decrease in shear stiffness at the joints between the rings,uplift is typically observed as bending and dislocation deformation at these joints.Existing modeling methods typically rely on the Euler-Bernoulli beam theory,only considering the bending effect while disregarding shear deformation.Furthermore,the constraints on the shield tail are often neglected in existing models.In this study,an improved theoretical model of tunnel floating is proposed.The constraint effect of the shield machine shell on the tunnel structure is considered using the structural forms of two finite long beams and one semi-infinite long beam.Furthermore,the Timoshenko beam theory is adopted,providing a more accurate description of tunnel deformation,including both the bending effect and shear deformation,than existing models.Meanwhile,the buoyancy force and stratum resistance are calculated in a nonlinear manner.A reliable method for calculating the shear stiffness correction factor is proposed to better determination of the calculation parameters.The proposed theoretical model is validated through five cases using sitemonitored data.Its applicability and effectiveness are demonstrated.Furthermore,the influences of soil type,buried depth,and buoyancy force on the three key indicators of tunnel floating(i.e.the maximum uplift magnitude,the ring position with the fastest uplift race,and the ring position with the maximum uplift magnitude)are analyzed.The results indicate that the proposed model can provide a better understanding of the floating characteristics of the tunnel structure during construction. 展开更多
关键词 Analytical solution Conceptual model Matrix transfer method Shield tunnel Timoshenko beam theory Tunnel uplift
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Thermal and exhumation history of the Songnan Low Uplift,Qiongdongnan Basin:constraints from the apatite fission-track and zircon(U-Th)/He thermochronology
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作者 Xiaoyin Tang Kaixun Zhang +3 位作者 Shuchun Yang Shuai Guo Xinyan Zhao Zhizhao Bai 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2024年第4期40-49,共10页
Significant advancements have been made in the study of Mesozoic granite buried hills in the Songnan Low Uplift(SNLU)of the Qiongdongnan Basin.These findings indicate that the bedrock buried hills in this basin hold g... Significant advancements have been made in the study of Mesozoic granite buried hills in the Songnan Low Uplift(SNLU)of the Qiongdongnan Basin.These findings indicate that the bedrock buried hills in this basin hold great potential for exploration.Borehole samples taken from the granite buried hills in the SNLU were analyzed using apatite fission track(AFT)and zircon(U-Th)/He data to unravel the thermal history of the basement rock.This information is crucial for understanding the processes of exhumation and alteration that occurred after its formation.Thermal modeling of a sample from the western bulge of the SNLU revealed a prolonged cooling event from the late Mesozoic to the Oligocene period(~80-23.8 Ma),followed by a heating stage from the Miocene epoch until the present(~23.8 Ma to present).In contrast,the sample from the eastern bulge experienced a more complex thermal history.It underwent two cooling stages during the late Mesozoic to late Eocene period(~80-36.4 Ma)and the late Oligocene period(~30-23.8 Ma),interspersed with two heating phases during the late Eocene to early Oligocene period(~36.4-30 Ma)and the Miocene epoch to recent times(~23.8-0 Ma),respectively.The differences in exhumation histories between the western and eastern bulges during the late Eocene to Oligocene period in the SNLU can likely be attributed to differences in fault activity.Unlike typical passive continental margin basins,the SNLU has experienced accelerated subsidence after the rifting phase,which began around 5.2 Ma ago.The possible mechanism for this abnormal post-rifting subsidence may be the decay or movement of the deep thermal source and the rapid cooling of the asthenosphere.Long-term and multi-episodic cooling and exhumation processes play a key role in the alteration of bedrock and contribute to the formation of reservoirs.On the other hand,rapid post-rifting subsidence(sedimentation)promotes the formation of cap rocks. 展开更多
关键词 granite buried hills (U-Th)/He dating fission-track dating EXHUMATION Songnan Low uplift
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AI机器学习:体育消费实验Uplift因果模型研究
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作者 张敖玮 殷亚光 +2 位作者 成瀚宇 唐琳 李星民 《体育科技文献通报》 2024年第4期169-172,共4页
2019年Metalearners for Estimating Heterogeneous Treatment Effects using Machine Learning的发表引发了世界因果推断理论的研究热情。目前,机器学习与因果推断论中的许多统计模型已被广泛应用。本文采用文献资料法、数理统计分析... 2019年Metalearners for Estimating Heterogeneous Treatment Effects using Machine Learning的发表引发了世界因果推断理论的研究热情。目前,机器学习与因果推断论中的许多统计模型已被广泛应用。本文采用文献资料法、数理统计分析方法、案例研究法等研究方法,研究推演现代因果推断理论中较为知名的Uplift因果模型在体育中的应用场景,其中Uplift因果模型包括S-learner(单模型)、T-learner(双模型)、X-learner(交叉训练模型)。结果显示,在体育消费随机对照实验中应用Uplift因果模型,可以基于基本模型进一步推导出各变量因素之间的因果关系,验证并分析自变量对因变量变化的影响;率先在体育消费市场研究与实验中应用Uplift因果模型可以填补我国体育消费实验数据分析方法的空缺。 展开更多
关键词 AI 机器学习 元分析 体育消费 uplift因果模型
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Uplift算法在商业银行智能营销体系中的应用研究
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作者 赵靓 高龙 +1 位作者 郭苏娴 刘书芳 《金融科技时代》 2024年第11期15-23,共9页
当今时代,商业银行将大量机器学习模型应用于客户营销领域中,但传统的机器学习模型仅预测客户AUM是否提升或客户是否购买某产品,无法区分提升与营销间的因果关系。针对当前商业银行在智能营销方面的不足,文章深入探索了Uplift模型在商... 当今时代,商业银行将大量机器学习模型应用于客户营销领域中,但传统的机器学习模型仅预测客户AUM是否提升或客户是否购买某产品,无法区分提升与营销间的因果关系。针对当前商业银行在智能营销方面的不足,文章深入探索了Uplift模型在商业银行营销端的实践应用。以X商业银行数据为基础,文章构建了与Uplift模型相匹配的智能营销体系,并设计了合理的评估指标体系。通过实证研究,发现以X-Learner为代表的Uplift模型在评估指标上表现优异,显著提高了营销的精准性和效率,为商业银行降本增效提供了有效手段。本研究不仅为商业银行的智能营销提供了新的视角和方法论,也为Uplift算法在更广泛领域的应用提供了有益的参考。 展开更多
关键词 uplift 商业银行 智能营销
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Exploring the rules of cropland elevation uplift in China 被引量:2
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作者 YUAN Jin-tao CHEN Wan-xu +1 位作者 ZENG Jie YE Xin-yue 《Journal of Mountain Science》 SCIE CSCD 2023年第7期1824-1841,共18页
Cropland elevation uplift(CLEU) has recently become a new challenge for agricultural modernization,food security,and sustainable cropland use in China.Uncovering the rules of CLEU is of great theoretical and practical... Cropland elevation uplift(CLEU) has recently become a new challenge for agricultural modernization,food security,and sustainable cropland use in China.Uncovering the rules of CLEU is of great theoretical and practical significance for China’s sustainable agricultural development and rural revitalization strategy.However,existing studies lack in-depth disclosure of multi-scale CLEU evolution rules,making it difficult to support the formulation of specific cropland protection policies.We analyzed the spatio-temporal evolution and multiscale CLEU in China from 1980 to 2020 using the Lorenz curve,gravity center model,hotspot analysis,and cropland elevation spectrum.The results indicated that the center of gravity of cropland moved to the northeast from 1980 to 2000 and then shifted to the northwest.The spatial distribution of cropland became increasingly imbalanced from 1980 to 2000.The change hotspots clustered in the northwest and the northeast,whereas cold-spots were mainly in southeastern China.The average elevation of cropland increased by 17.38 m,and the elevation uplift rule in different regions differed evidently across scales.From 1980 to 2000,all provinces except Xinjiang,Inner Mongolia,Gansu,and Yunnan exhibited CLEU,with Qinghai,Tibet,Beijing,and Guangdong showing the most noticeable uplifting.The CLEU can alleviate the shortage of cropland to some extent.However,without a planning constraint,the CLEU will lead to the increase of ecological risk and food security risk. 展开更多
关键词 CROPLAND Elevation uplift rules MULTI-SCALE Elevation spectrum China
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Failure of levees induced by toe uplift:Investigation of post-failure behavior using material point method 被引量:1
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作者 Veronica Girardi Francesca Ceccato +2 位作者 Alex Rohe Paolo Simonini Fabio Gabrieli 《Journal of Rock Mechanics and Geotechnical Engineering》 SCIE CSCD 2023年第4期970-983,共14页
Levees are essential structures in flood defense systems,and their failures can lead to devastating consequences on the surrounding territories.One of the failure mechanisms mostly controlled by the foundation soil st... Levees are essential structures in flood defense systems,and their failures can lead to devastating consequences on the surrounding territories.One of the failure mechanisms mostly controlled by the foundation soil stratigraphy is the instability of the land side slope,triggered by the development of high uplift pressures in the foundation.This complex phenomenon has been investigated experimentally with centrifuge tests or large-scale tests and numerically with the limit equilibrium method(LEM)and the finite element method(FEM).In this work,we applied a multiphase formulation of the material point method(MPM)to analyze the development of toe uplift instability mechanism,from the onset of failure to large displacements.The numerical model is inspired by an experiment carried out in a geotechnical centrifuge test by Allersma and Rohe(2003).The comparison with the experiment allows for understanding critical pore pressure triggering large displacements in the foundation soils.Moreover,we numerically evaluated the impact of different values of foundation soils’hydraulic conductivity on the failure mechanism.The results show that hydraulic conductivity mainly influences the time of failure onset and the extension of shear localization at depth.Finally,the advantages of using large displacement approaches in the safety assessment of earth structures are discussed.Unlike FEM,there are no issues with element distortions generating difficulties with numerical convergence,allowing for full postfailure reproduction.This capability permits precise quantification of earth structure damages and post-failure displacements.The ensuing reinforcement systems’design is no longer over-conservative,with a significant reduction in associated costs. 展开更多
关键词 Slopes safety assessment LEVEES uplift pressure Large deformation analysis
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Texture development of mesophase in reservoir pyrobitumen and the temperature-pressure converting of the gas reservoir in the Chuanzhong Uplift, Southwestern China
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作者 Cheng-Yu Yang Mei-Jun Li +3 位作者 Tie-Guan Wang Ning-Ning Zhong Rong-Hui Fang Long Wen 《Petroleum Science》 SCIE EI CAS CSCD 2023年第2期721-732,共12页
The Neoproterozoic-Lower Paleozoic dolostone gas reservoirs in the Chuanzhong Uplift in Southwestern China contain the mesophase pyrobitumen (pyrobitumen with mesophase). The mesophase in the pyrobitumen is mostly com... The Neoproterozoic-Lower Paleozoic dolostone gas reservoirs in the Chuanzhong Uplift in Southwestern China contain the mesophase pyrobitumen (pyrobitumen with mesophase). The mesophase in the pyrobitumen is mostly composed of a mixture of condensed macromolecule polycyclic aromatic hydrocarbons (PAH), and has been mostly converted to various grain, flow, and domain textures. The volcanic activity nearby the Chuanzhong Uplift may have generated very hot (over 300 °C) hydrothermal fluid, with migration of the fluid into the dolostone reservoir transforming the hydrocarbons in the reservoir into an anisotropic carbon by-product, which formed under high temperature and pressure conditions;over 300 °C and 200 MPa according to fluid inclusion analysis. The high temperature-pressure in reservoir was caused by sudden devolatilization of the hydrocarbons due to hydrothermal heating, which formed the unusual texture of the mesophase. The elliptical mesophase grains (EG), the honeycomb structure of pyrobitumen, and the occurrence of polarized classes of mesophase in single pyrobitumen deposits are all unusual textures. This study investigates the texture development of this pressure-affected pyrobitumen. Observation and study of the mesophase suggest that the class of mesophase in pyrobitumen is determined by temperature, while pressure (assessed from associated fluid inclusions) significantly affected the texture. Analysis of the texture of the pyrobitumen in conjunction with previous thermometry results from methane inclusions suggests that the high class mesophase of the pyrobitumen could be applied as a temperature indicator for geological conditions. Furthermore, the unusual textures of the pyrobitumen including elliptical mesophase grains (EG), the honeycomb structure of pyrobitumen, and the occurrence of polarized classes of mesophase in single pyrobitumen could reflect the abnormal high formation pressure. 展开更多
关键词 PYROBITUMEN MESOPHASE Optical texture Pressure affect Oil reservoir Chuanzhong uplift
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新疆准噶尔盆地白家海凸起深部煤层气勘探开发进展及启示 被引量:3
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作者 兰浩 杨兆彪 +4 位作者 仇鹏 王彬 刘常青 梁宇辉 王钰强 《煤田地质与勘探》 EI CAS CSCD 北大核心 2024年第2期13-22,共10页
白家海凸起侏罗系煤是国内深部煤层气直井产量很早取得突破的地方,为准噶尔盆地的重要靶区。煤储层为特低灰、低水分、中高挥发性煤,孔渗系统较好。具有“古生新储”和“自生自储”两种成藏模式,煤层含气量高、游离气占比高、含气饱和度... 白家海凸起侏罗系煤是国内深部煤层气直井产量很早取得突破的地方,为准噶尔盆地的重要靶区。煤储层为特低灰、低水分、中高挥发性煤,孔渗系统较好。具有“古生新储”和“自生自储”两种成藏模式,煤层含气量高、游离气占比高、含气饱和度高,为优质煤层气储层。历经多年的勘探开发证明:多数直井试采无需排水降压即可快速见气(2~5 d),排采初期日产气量较高(2100~9890 m^(3)),日产水量少甚至不产水(<5 m^(3)),可自喷生产,返排率低,长期试采压力均衡下降,且具有一定的稳产期(25~60 d);煤层射孔层厚度、压裂液体系、压裂加砂比均可影响煤层气试气效果,其中冻胶、胍胶体系优于活性水-清洁压裂液体系。最新施工的彩探1H水平井试采表现出压裂开井后即高产,试采最高日产气量5.7万m^(3),日产水量少(0.5~3.0 m^(3)),表现出常规天然气特征,随后衰减稳定,表现为吸附气与游离气共同产出;与直井对比,水平井产量高、稳产时间长、压降速率小。基于研究区储层特征和含气性特征,及勘探开发历程,得到3方面启示。一是深部多类型气藏富集规律再认识:需重视油气运聚圈闭的成藏演化研究,重视深部位气水空间分配和富集规律的研究。二是深部中低阶煤储层可压性评价:针对凸起高部位孔渗系统好的中低煤阶储层,需形成适合的压裂工艺体系。三是深部多类型气藏开发方式优化:针对游离气占比高的气藏,实现游离气-吸附气的接续产出,保持降压面积稳定扩展,排采控制尤为关键。 展开更多
关键词 准噶尔盆地 白家海凸起 深部煤层气 孔渗系统 成藏特征 勘探开发进展
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滨里海盆地东缘北特鲁瓦油田石炭系层序地层与沉积演化特征 被引量:2
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作者 陈烨菲 赵伦 +3 位作者 侯珏 李毅 王淑琴 李建新 《古地理学报》 CAS CSCD 北大核心 2024年第1期58-74,共17页
根据三维地震、测井及钻井取心等资料,结合Vail的层序划分方案,在滨里海盆地东缘北特鲁瓦油田石炭系碳酸盐岩台地内识别出7个地震层序界面及7个钻井层序界面,并将KT-Ⅰ油层组划分为3个半三级层序,KT-Ⅱ油层组划分为3个三级层序。纵向上... 根据三维地震、测井及钻井取心等资料,结合Vail的层序划分方案,在滨里海盆地东缘北特鲁瓦油田石炭系碳酸盐岩台地内识别出7个地震层序界面及7个钻井层序界面,并将KT-Ⅰ油层组划分为3个半三级层序,KT-Ⅱ油层组划分为3个三级层序。纵向上层序格架内沉积环境由开阔台地、局限台地至蒸发台地演化。根据研究区层序格架内的古地貌恢复及沉积演化研究,将研究区古地貌—沉积演化划分为3个阶段:台地初始隆坳分异期(SQ2-SQ3层序)、差异抬升与沉积分异定型期(SQ4层序)及继承发育期(SQ5-SQ7层序)。进一步分析认为,层序格架控制下的隆坳格局分异控制了白云岩亚类在平面上的分布,低部位以泥晶云岩—膏盐岩组合和泥晶云岩—泥晶灰岩组合为主,主要为潟湖相沉积;而高部位则以泥粉晶云岩、细粉晶云岩和残余颗粒泥晶云岩为主,发育云坪相及云化颗粒滩相沉积。结果表明,区内KT-Ⅰ油层组沉积期并非前人认为的西高东低剥蚀后沉降充填,而是继承性差异沉降的结果,古地理格局总体具有“东台西槽、北高南低”特征,其始终控制着有利相带和优质储集层的发育展布。这一认识对滨里海地区油气勘探开发战略选区具有重要的指导作用。 展开更多
关键词 层序地层 古地貌—沉积演化 隆坳分异 碳酸盐岩台地 石炭系 北特鲁瓦油田 滨里海盆地
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泸州地区五峰组——龙马溪组页岩气成藏特征 被引量:2
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作者 刘洪林 王怀厂 李晓波 《新疆石油地质》 CAS CSCD 北大核心 2024年第1期19-26,共8页
为寻找四川盆地泸州地区五峰组—龙马溪组页岩气有利区,在开展流体包裹体检测、页岩微观孔隙观测、气泡变孔模拟等研究基础上,查明了泸州地区构造埋藏过程和生烃热演化过程,总结了泸州地区页岩气成藏特征和成藏规律。研究结果表明:泸州... 为寻找四川盆地泸州地区五峰组—龙马溪组页岩气有利区,在开展流体包裹体检测、页岩微观孔隙观测、气泡变孔模拟等研究基础上,查明了泸州地区构造埋藏过程和生烃热演化过程,总结了泸州地区页岩气成藏特征和成藏规律。研究结果表明:泸州地区五峰组—龙马溪组富有机质页岩厚度大,在二叠纪—早三叠世生油,经历了中三叠世和燕山运动期—喜马拉雅运动期2次构造抬升,中三叠世抬升幅度有限,未导致大规模烃散失,燕山运动期—喜马拉雅运动期构造抬升晚于川东南且幅度小,利于页岩气保存;泸州地区五峰组—龙马溪组页岩有机孔发育,是由于中三叠世隆升时间短,强度小,未发生大规模排烃,大量液态烃保留在储集层中,有利于后期有机孔的大量形成,同时在晚三叠世—中白垩世,地层深埋发生液态烃裂解产气,地层广泛超压,有利于有机孔的后期保存;泸州地区三叠纪隆升虽然时间短、强度小,但是从模拟实验结果来看,可以导致原油稠化和气孔形成,对页岩气富集成藏有利。因此,发生在印支运动期的泸州地区的隆升造成原油稠化,有利于页岩气富集成藏;泸州地区地层抬升时间晚,页岩气散失时间短,低角度层理缝发育,而纵向裂缝少,均有利于形成超压页岩气富集区。提出的泸州地区五峰组—龙马溪组页岩富集成藏规律,对于指导其他同类型油气勘探具有借鉴意义。 展开更多
关键词 四川盆地 泸州地区 五峰组 龙马溪组 页岩储集层 页岩气 孔隙成因 隆升 成藏
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Geochemical characteristics of Sr isotopes in the LS33 drill core from the Qiongdongnan Basin, South China Sea, and their response to the uplift of the Tibetan Plateau
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作者 Ke Wang Shikui Zhai +1 位作者 Zenghui Yu Huaijing Zhang 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2023年第5期117-129,共13页
Making full use of modern analytical and testing techniques to explore and establish new indexes or methods for extracting paleoseawater geochemical information from sediments will help to reconstruct the sedimentary ... Making full use of modern analytical and testing techniques to explore and establish new indexes or methods for extracting paleoseawater geochemical information from sediments will help to reconstruct the sedimentary paleoenvironment in different research areas.The connection between the subsidence of the South China Sea basin and the uplift of the Tibetan Plateau has been a scientific concern in recent decades.To explore the information on the sedimentary paleoenvironment,provenance changes and uplift of Tibetan Plateau contained in core sediments(debris),we selected core samples from Well LS33 in the Qiongdongnan Basin,South China Sea,and analyzed the contents of typical elements(Al,Th,and rare earth elements)that can indicate changes in provenance and the Sr isotopic compositions,which can reveal the geochemical characteristics of the paleoseawater depending on the type of material(authigenic carbonate and terrigenous detritus).The results show the following:(1)during the late Miocene,the Red River transported a large amount of detrital sediments from the ancient continental block(South China)to the Qiongdongnan Basin.(2)The authigenic carbonates accurately record changes in the 87Sr/86Sr ratios in the South China Sea since the Oligocene.These ratios reflect the semi-closed marginal sea environment of the South China Sea(relative to the ocean)and the sedimentary paleoenvironment evolution process of the deep-water area of the Qiongdongnan Basin from continental to transitional and then to bathyal.(3)Since the Neogene,the variations in the 87Sr/86Sr ratio in the authigenic carbonates have been consistent with the variations in the uplift rate of the Tibetan Plateau and the sediment accumulation rate in the Qiongdongnan Basin.These consistent changes indicate the complex geological process of the change in the rock weathering intensity and terrigenous Sr flux caused by changes in the uplift rate of the Tibetan Plateau,which influence the Sr isotope composition of seawater. 展开更多
关键词 sediments from a drill core grouping analysis elements and Sr isotopes provenance and paleoenvironment uplift of the Tibetan Plateau and subsidence of the South China Sea basin
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希夏邦马峰地区始新世地壳加厚和隆升过程 被引量:3
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作者 王佳敏 侯康师 +1 位作者 李潇丽 吴福元 《岩石学报》 SCIE EI CAS CSCD 北大核心 2024年第5期1429-1445,共17页
中新世中期之前喜马拉雅山脉的隆升历史和深部动力机制,还存在极大的争议、缺乏基本的数据约束。喜马拉雅造山带核部高级变质岩的埋藏和折返过程可以约束地壳加厚和山脉隆升过程,但是现有的变质记录主要为渐新世晚期-中新世中期,始新世... 中新世中期之前喜马拉雅山脉的隆升历史和深部动力机制,还存在极大的争议、缺乏基本的数据约束。喜马拉雅造山带核部高级变质岩的埋藏和折返过程可以约束地壳加厚和山脉隆升过程,但是现有的变质记录主要为渐新世晚期-中新世中期,始新世变质作用的分布范围、形成过程和地质意义仍然未被充分挖掘。本文首先厘定了希夏邦马峰(8027m)山体的基本岩石组成:下部为高喜马拉雅正/副片麻岩,上部为肉切村群变粒岩及贯入其中的淡色花岗岩席。进一步对1964年希夏邦马峰登山科考采集的眼球状片麻岩进行了变质作用相平衡模拟和独居石微区原位U-Th-Pb定年,确定了始新世变质记录的P-T-t演化轨迹:M1阶段中P/T型变质压力峰期,条件为~1.0GPa、~740℃(~22℃/km),变质年龄为~37Ma;后近等温降压至M2阶段低P/T型变质温度峰期,条件为0.5~0.4GPa、~760℃(45~57℃/km),变质年龄为~25Ma;在~18Ma左右冷却至固相线以下。希夏邦马峰~37Ma的中P/T型变质和地壳加厚事件与北喜马拉雅穹隆、高喜马拉雅主体、前陆飞来峰等地区的记录一致(40~37Ma,20~25℃/km),表明印度-亚洲初始碰撞约20Myr后中上地壳被堆叠埋藏至>33km以下,发生了广泛的整体性加厚和深熔作用。该事件与喜马拉雅内陆残留海最终退却的时间吻合,是喜马拉雅山脉初始隆升的诱因。喜马拉雅山脉不是晚新生代以来隆升的,而是经历了自始新世中期以来的长期地壳堆叠和隆升过程。 展开更多
关键词 喜马拉雅 初始隆升 地壳加厚 中P/T型变质作用 独居石U-Th-Pb岩石年代学
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An Orthogonal Collision Dynamic Mechanism of Wave-Like Uplift Plateaus in Southern Asia
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作者 Weihong Qian Jeremy Cheuk-Hin Leung Banglin Zhang 《Open Journal of Geology》 2023年第8期828-846,共19页
In southern Asia, there are three large-scale wave-like mountains ranging from the Tibetan Plateau westward to the Iranian Plateau and the Armenian Plateau. On the southern side between plateaus, there are the Indian ... In southern Asia, there are three large-scale wave-like mountains ranging from the Tibetan Plateau westward to the Iranian Plateau and the Armenian Plateau. On the southern side between plateaus, there are the Indian Peninsula and the Arabian Peninsula. What dynamic mechanisms form the directional alignment of the three plateaus with the two peninsulas remains a mystery. In the early stages of the Earth’s geological evolution, the internal structure of the Earth was that the center was a solid core, and the outmost layer was a thin equatorial crust zone separated by two thick pristine continents in polar areas, while the middle part was a deep magma fluid layer. Within the magma fluid layer, thermal and dynamic differences triggered planetary-scale vertical magma cells and led to the core-magma angular momentum exchange. When the core loses angular momentum and the magma layer gains angular momentum, the movement of upper magma fluids to the east and the tropical convergence zone (TCZ) drives the split and drift of two thick pristine continents, eventually forming the current combination of these plateaus and peninsulas and their wave-like arrangement along the east-west direction. Among them, the horizontal orthogonal convergence (collision) of upper magma fluids from the two hemispheres excited the vertical shear stress along the magma TCZ, which is the dynamic mechanism of mountain uplifts on the north side and plate subductions on the south side. To confirm this mechanism, two examples of low-level winds are used to calculate the correspondence between cyclone/anticyclonic systems generated by the orthogonal collision of airflows along the atmospheric TCZ and satellite-observed cloud systems. Such comparison can help us revisit the geological history of continental drift and orogeny. 展开更多
关键词 Plateau uplift Plate Subduction Tibetan Plateau Iranian Plateau Armenian Plateau
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建筑结构隔震技术研究进展 被引量:1
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作者 潘鹏 曾一 +2 位作者 曹迎日 艾华浩 王海深 《工程力学》 EI CSCD 北大核心 2024年第5期39-54,共16页
建筑结构隔震技术通过在建筑结构底部或中间楼层设置隔震装置,延长结构的自振周期,并提供适当的阻尼使得结构的响应大幅度减小,能够更有效地保护房屋结构以及室内设备的安全,可显著提升建筑震后功能可恢复能力。目前建筑结构隔震技术已... 建筑结构隔震技术通过在建筑结构底部或中间楼层设置隔震装置,延长结构的自振周期,并提供适当的阻尼使得结构的响应大幅度减小,能够更有效地保护房屋结构以及室内设备的安全,可显著提升建筑震后功能可恢复能力。目前建筑结构隔震技术已经有较为成熟的技术产品和工程应用,已广泛应用于住宅、医院、学校、博物馆和图书馆等建筑中。随着《建设工程抗震管理条例》的颁布,预期隔震技术将有更广阔的应用场景。隔震建筑也将逐步从低层、简单建筑结构向高层、复杂建筑结构的方向发展。目前常用的隔震装置存在着抗拉能力不足、对竖向地震或竖向环境振动减振效果不足、控制频宽窄、适应性不足以及使用状态及损伤状态难以监测等问题。为此,众多学者针对以上问题进行了深入研究,开发了抗拉隔震支座、三维隔震(振)支座、半主动隔震支座和隔震支座的健康监测系统,为扩展隔震技术的应用范围提供了解决方法。目前,相关研究偏重于新型隔震装置的性能研究,未来应全面考虑新型隔震装置对于建筑的影响,提出配套的设计方法,并进行示范性工程应用,加快隔震技术的推广。 展开更多
关键词 隔震技术 抗拉支座 三维隔震(振)支座 半主动隔震系统 健康监测 综述
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吕梁古隆起对鄂尔多斯盆地马家沟组沉积的控制作用:基于陕西府谷剖面
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作者 丁晓琪 田胤瑜 +3 位作者 雷涛 张威 李晓慧 高景云 《古地理学报》 CAS CSCD 北大核心 2024年第3期671-682,共12页
中奥陶世马家沟组沉积时期,鄂尔多斯局限海周缘分布着一系列古隆起,其中吕梁古隆起对马家沟组沉积的控制作用研究相对薄弱,制约了对鄂尔多斯盆地东北部马家沟组沉积环境的认识。通过对陕西府谷剖面实测和采样,结合鄂尔多斯盆地北部的钻... 中奥陶世马家沟组沉积时期,鄂尔多斯局限海周缘分布着一系列古隆起,其中吕梁古隆起对马家沟组沉积的控制作用研究相对薄弱,制约了对鄂尔多斯盆地东北部马家沟组沉积环境的认识。通过对陕西府谷剖面实测和采样,结合鄂尔多斯盆地北部的钻井、取心资料,分析了马家沟组的厚度、岩相类型及沉积微相变化,总结出吕梁古隆起对马家沟组沉积的控制作用。控制作用主要表现为:(1)吕梁古隆起的间歇性活动阻隔了鄂尔多斯局限海与华北广海的海水循环;(2)高海平面期,吕梁古隆起位于水下,对海水的阻隔作用弱,且古隆起区为开阔海灰坪,古隆起以西地层厚度变化较小,形成灰坪和云坪的沉积分异;(3)低海平面期,吕梁古隆起间歇性暴露,海水循环被明显阻隔,且古隆起区为潮间—潮上带的泥云坪,向东地层厚度减小,过渡为灰坪,而向西地层厚度迅速增加,形成泥云坪、膏云坪、膏盐湖的沉积分异。该研究成果为鄂尔多斯盆地北部马家沟组的沉积学研究提供了相关的岩石学和古环境方面的证据。 展开更多
关键词 吕梁古隆起 古岩溶 白云岩 马家沟组 鄂尔多斯盆地
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深地震反射剖面揭示沧县隆起和黄骅坳陷及邻区的地壳精细结构和构造特征
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作者 秦晶晶 刘保金 +4 位作者 酆少英 徐锡伟 田一鸣 朱国军 左莹 《地震地质》 EI CSCD 北大核心 2024年第3期608-626,共19页
为研究华北盆地的地壳精细结构和断裂的深、浅构造关系,跨冀中坳陷、沧县隆起、黄骅坳陷和埕宁隆起完成了1条长约200km的深地震反射剖面和1条长66km的中-浅层地震反射剖面。结果表明,沿剖面地壳厚30~35km,且具有东薄西厚的分布特征,在... 为研究华北盆地的地壳精细结构和断裂的深、浅构造关系,跨冀中坳陷、沧县隆起、黄骅坳陷和埕宁隆起完成了1条长约200km的深地震反射剖面和1条长66km的中-浅层地震反射剖面。结果表明,沿剖面地壳厚30~35km,且具有东薄西厚的分布特征,在冀中坳陷下方,莫霍面出现明显上隆,其隆起幅度为2~3km。研究区上地壳反射结构具有凹隆相间的展布特征,多条规模较大的断裂隐伏于华北盆地之下,对该区隆起和坳陷的形成与发展具有重要的控制作用。剖面上一系列与主断裂同向或反向的次级断裂将研究区的上地壳切割为多个次级小型地堑或半地堑断陷,导致整个华北盆地的上地壳结构复杂化。下地壳反射结构由一系列反射能量变化较大、横向上不能稳定成层、产状复杂多变的反射事件构成,这与反射能量强、横向连续性好及产状近水平展布的上地壳反射明显不同,暗示研究区上、下地壳物质有着明显不同的形成环境、变形方式和温压条件。中-浅层地震剖面和深地震反射剖面共同揭示的太行山山前断裂表现为一条低角度的大型铲形正断层,向下可与太行山东缘向E缓倾的大型滑脱构造(拆离断层)相联系;沧西断裂、沧东断裂和埕西断裂作为沧县隆起、黄骅坳陷、埕宁隆起的边界断裂,控制了该区堑、垒构造的形成与发展,是第四纪以来的隐伏活动断裂,推测其深部终止于深约18km的壳内解耦面上。文中研究结果可为进一步理解华北盆地的深部动力学过程及分析研究区深、浅断裂构造关系提供地震学依据。 展开更多
关键词 沧县隆起 黄骅坳陷 冀中坳陷 深地震反射剖面 地壳结构和构造
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忻定盆地金山凸起东缘断裂展布及晚第四纪最新活动特征
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作者 扈桂让 闫小兵 +3 位作者 梁瑞平 任瑞国 薛晓东 张丽 《大地测量与地球动力学》 CSCD 北大核心 2024年第6期606-610,共5页
通过野外地质地貌调查结合无人机航拍测量、地质雷达勘探及浅层地震勘探综合分析认为,金山凸起东缘断裂整体呈NE向展布,走向40°,北起忻口村一带,向SW经金山铺村西、前淤泥村西延伸至部落村以北,进而向SWS转折进入盆地区。经探槽开... 通过野外地质地貌调查结合无人机航拍测量、地质雷达勘探及浅层地震勘探综合分析认为,金山凸起东缘断裂整体呈NE向展布,走向40°,北起忻口村一带,向SW经金山铺村西、前淤泥村西延伸至部落村以北,进而向SWS转折进入盆地区。经探槽开挖和年龄测试,该断裂段最新断错晚更新世早期地层。 展开更多
关键词 忻定盆地 金山凸起东缘断裂 晚第四纪 活动性 活动断层
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准噶尔盆地中拐凸起南部构造演化及油气地质意义——以中佳地区下二叠统佳木河组为例
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作者 李道清 兰浩 +3 位作者 郭巧珍 陈河青 汪洋 仇鹏 《东北石油大学学报》 CAS 北大核心 2024年第5期48-61,I0004,共15页
准噶尔盆地中拐凸起南部中佳地区佳木河组多口井获工业气流,断裂对油气影响显著。利用三维地震和钻井资料,采用平衡演化剖面技术,分析中拐凸起南部断裂发育特征及演化过程,建立断裂与下二叠统佳木河组二段油气成藏成储的联系。结果表明... 准噶尔盆地中拐凸起南部中佳地区佳木河组多口井获工业气流,断裂对油气影响显著。利用三维地震和钻井资料,采用平衡演化剖面技术,分析中拐凸起南部断裂发育特征及演化过程,建立断裂与下二叠统佳木河组二段油气成藏成储的联系。结果表明:中拐凸起南部主要发育逆冲断裂、走滑断裂和正断裂。逆冲断裂在早二叠世晚期开始发育,晚二叠世停止发育,对下二叠统佳木河组二段改造作用显著;走滑断裂集中在三叠纪发育,对地层的改造作用有限;正断裂在三叠系层内发育,未改造佳木河组。研究区构造演化可划分为4个阶段:石炭纪—二叠纪逆冲改造阶段、三叠纪—侏罗纪压扭走滑阶段、侏罗纪—白垩纪隆升剥蚀阶段和白垩纪—新近纪沉积掀斜阶段。石炭纪—二叠纪是断裂发育的主要时期;佳木河组二段优质储层主要发育于近断裂位置,断裂发育位置与研究区单斜构造共同控制油气圈闭的分布和形成;断裂与不整合分别为油气提供纵向和横向运移通道,将油气藏由北向南划分为低饱和度气顶大油环区、小气顶大油环区、小油环大凝析气藏区、无油环凝析气藏区及纯气区5种类型。该结果为中拐凸起南部中佳地区下二叠统佳木河组油气勘探部署提供指导。 展开更多
关键词 准噶尔盆地 中拐凸起 佳木河组 构造演化 断裂体系 “甜点”分布
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