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Geologic hazard susceptibility assessment based on statistical optimization and machine learning: A case study of the Loess Plateau, Shaanxi Province, northwestern China 基于统计优化和机器学习的地质灾害易感性评价——以陕西黄土高原为例
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-01 Epub Date: 2026-02-20 DOI: 10.31035/cg2024093
Hao Cheng , Zhen-kai Zhang , Zeng-lin Hong , Wen-long Zhang , Hong-quan Teng , Shuai Yang , Zi-yao Wang , Yu-xuan Dong
This study developed a modeling methodology for statistical optimization-based geologic hazard susceptibility assessment, aiming to enhance the comprehensive performance and classification accuracy of the assessment models. First, the cumulative probability method revealed that a low probability (15%) of geologic hazards between any two geologic hazard points occurred outside a buffer zone with a radius of 2297 m (i.e., the distance threshold). The training dataset was established, consisting of negative samples (non-hazard points) randomly generated based on the distance threshold, positive samples (i.e., historical hazards), and 13 conditioning factors. Then, models were built using five machine learning algorithms, namely random forest (RF), gradient boosting decision tree (GBDT), naive Bayes (NB), logistic regression (LR), and support vector machine (SVM). The comprehensive performance of the models was assessed using the area under the receiver operating characteristic curve (AUC) and overall accuracy (OA) as indicators, revealing that RF exhibited the best performance, with OA and AUC values of 2.7127 and 0.981, respectively. Furthermore, the machine learning models constructed by considering the distance threshold outperformed those built using the unoptimized dataset. The characteristic factors were ranked using the mutual information method, with their scores decreasing in the order of rainfall (0.1616), altitude (0.06), normalized difference vegetation index (NDVI; 0.04), and distance from roads (0.03). Finally, the geologic hazard susceptibility classification was assessed using the natural breaks method combined with a clustering algorithm. The results indicate that the clustering algorithm exhibited higher classification accuracy than the natural breaks method. The findings of this study demonstrate that the proposed model optimization scheme can provide a scientific basis for the prevention and control of geologic hazards.
为提高地质灾害易感性评价模型的综合性能和分类精度,建立了基于统计优化的地质灾害易感性评价建模方法。首先,累积概率法发现,在半径为2297 m(即距离阈值)的缓冲带之外,任意两个地质灾害点之间发生地质灾害的概率较低(15%)。建立训练数据集,由基于距离阈值随机生成的负样本(非危害点)、正样本(即历史危害)和13个条件因子组成。然后,使用随机森林(RF)、梯度增强决策树(GBDT)、朴素贝叶斯(NB)、逻辑回归(LR)和支持向量机(SVM)五种机器学习算法建立模型。以受试者工作特征曲线下面积(AUC)和总体精度(OA)为指标对模型的综合性能进行评价,结果表明,RF模型的综合性能最好,OA和AUC分别为2.7127和0.981。此外,考虑距离阈值构建的机器学习模型优于使用未优化数据集构建的机器学习模型。利用互信息法对各特征因子进行排序,各特征因子得分依次为降雨(0.1616)、海拔(0.06)、归一化植被指数(NDVI; 0.04)、距离道路(0.03)。最后,采用自然断裂法结合聚类算法对地质灾害易感性进行分类。结果表明,该聚类算法比自然断裂法具有更高的分类精度。研究结果表明,所提出的模型优化方案可为地质灾害防治提供科学依据。
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引用次数: 0
A comparative study on the apatite and zircon from the ore-related and -barren magmatic rocks of the Shatanjiao region, Lower Yangtze River Belt: Controlling effects for petrogenesis and Cu-Au mineralization 长江下游沙滩角地区与贫矿岩浆岩中磷灰石和锆石的对比研究:对岩石成因和铜金矿化的控制作用
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-01 Epub Date: 2026-02-20 DOI: 10.31035/cg2024105
Yu Wang , Jing-ya Cao , Sheng-xiong Yang , Xiao-yong Yang , Majid Ghasemi Siani , Asghar Dolati , Muhammad Hafeez
The links between the adakitic rocks and Cu-Au mineralization have long been argued. This study investigates petrogenesis and its link to mineralization potential by a series of in-situ geochronological and geochemical signatures of apatite and zircon in three ore-related intrusions and one-barren intrusion in the Middle-Lower Yangtze River Metallogenic Belt (MLYRB). Zircon U-Pb dating yield ages of 139–143 Ma and 121 Ma for the ore-related and ore-barren intrusions, respectively. The ore-related rocks have higher apatite Sr/Y (1.57–9.69), (La/Yb)N (16.7–159.5), and δEu (0.45–0.74) than the ore-barren rocks of 0.57–1.02, 19.3–24.1 and 0.40–0.45, respectively, indicating the former has an adakitic affinity, while the latter has a non-adakitic affinity. The ore-related rocks have enriched zircon Hf isotopes with εHf(t) values of −15.9 to −5.5 and TDMC ages of 2408–1655 Ma and apatite Sr-Nd isotopes, indicating that the ore-related magmas were mainly originated from partial melting of subducted oceanic crust. The orebarren rocks have higher εHf(t) values of −6.6 to −4.6 and lower TDMC ages of 1598–1469 Ma and apatite Sr-Nd isotopes, indicating a lithospheric mantle source. The ore-related rocks have higher oxygen fugacity of mean ΔFMQ+2.00 and XF/XOH of 8.36–175 than the ore-barren rocks of mean ΔFMQ+1.43 and 3.72–4.96. It was inferred that magma source, water content, and oxygen fugacity emerge as critical factors governing the regional Cu-Au mineralization potential.
埃达克岩与铜金成矿作用之间的联系一直是争论的焦点。通过对长江中下游成矿带3个含矿侵入体和1个无矿侵入体中磷灰石和锆石的一系列原位年代和地球化学特征的研究,探讨了岩石成因及其与成矿潜力的联系。锆石U-Pb年龄分别为139 ~ 143 Ma和121 Ma。磷灰石Sr/Y(1.57 ~ 9.69)、(La/Yb)N(16.7 ~ 159.5)和δEu(0.45 ~ 0.74)分别高于贫矿岩(0.57 ~ 1.02)、(19.3 ~ 24.1)和(0.40 ~ 0.45),表明贫矿岩具有埃达质亲和性,而贫矿岩具有非埃达质亲和性。锆石Hf同位素富集,εHf(t)值为−15.9 ~−5.5,TDMC年龄为2408 ~ 1655 Ma,磷灰石Sr-Nd同位素富集,表明成矿岩浆主要来源于俯冲洋壳部分熔融。矿裸岩的εHf(t)值较高,为−6.6 ~−4.6,TDMC年龄较低,为1598 ~ 1469 Ma,磷灰石Sr-Nd同位素表明其为岩石圈地幔源。含矿岩的氧逸度平均值为ΔFMQ+2.00, XF/XOH值为8.36 ~ 175,高于贫矿岩的平均值ΔFMQ+1.43和3.72 ~ 4.96。岩浆来源、水含量和氧逸度是控制区域铜金成矿潜力的关键因素。
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引用次数: 0
Mineral resources of Asia continent: Resource endowment, mining industry pattern, and contributions to the world economy 亚洲大陆矿产资源:资源禀赋、矿业格局与对世界经济的贡献
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-01 Epub Date: 2026-02-20 DOI: 10.31035/cg2024127
Xi-feng Chen , Gang Wang , Yan-xiong Mei , Hai-jie Zhao , Yan-yun Ma
<div><div>Mineral resources in Asia continent and its mining industry play a significant role in the economic growth and industrialization of both Asia and the world. Asia continent boasts the most comprehensive kinds of minerals, with reserves of at least 38 of over 80 widely used minerals worldwide accounting for more than 30% of the global total reserves. Asia continent experienced three main tectonic evolution and mineralization stages: The Precambrian, the Paleozoic, and the Mesozoic to Cenozoic. The abundant mineral resources in this continent can be divided into seven first-order metallogenic belts (metallogenic domains), 18 second-order metallogenic belts (metallogenic provinces), 61 third-order metallogenic belts (metallogenic zones), and nine main minerogenetic series. Asia continent exhibits the most significant metallogenic specialization among all continents. Specifically, granite belts of Asia continent manifest pronounced metallogenic specialization of tin, rare metals, and porphyry Cu-Au-Mo deposits. Its maficultramafic rock belts and ophiolite belts display notable metallogenic specialization of lateritic nickel deposits and magmatic type chromite deposits, while its Mesozoic to Cenozoic basalt belts show remarkable metallogenic specialization of lateritic bauxite deposits. Consequently, many giant metallogenic belts were formed, including the Southeast Asian tin belt, the Qinghai-Xizang Plateau rare metal metallogenic belt, the Tethyan porphyry Cu-Au-Mo metallogenic belt, the circum-Pacific porphyry Cu-Au-Mo metallogenic belt, the Southeast Asian lateritic bauxite metallogenic belt, the Deccan Plateau lateritic bauxite metallogenic belt in India, the Southeast Asian lateritic nickel metallogenic belt, and the Tethyan magmatic type chromite metallogenic belt—all of which are significant metallogenic belts in Asia continent. Future mineral exploration in Asia should focus primarily on the Precambrian mineralization of ancient cratons, the Paleozoic mineralization of the Central Asian-Mongolian orogenic belt, and the Mesozoic to Cenozoic mineralization of the Tethyan and circum-Pacific mobile belts. Asia's mining industry not only underpins its own economic growth but also propels global economic development and industrialization, contributing significantly to the world economy. Asia boasts the highest production value of minerals, the largest annual production of minerals, and the greatest trade value of mineral products among all the continents, having emerged as the trade center of global mineral products and the center of the mining industry economy. China is identified as one of the few countries that possess the most comprehensive kinds of minerals, and its mining industry has supported and driven the economic development and industrialization of Asia and even the world. Standing as the largest mineral producer worldwide, China ranked first in the production of 28 mineral commodities in the world in 2022. Besides, China exhib
亚洲大陆的矿产资源及其采矿业在亚洲乃至世界的经济增长和工业化进程中发挥着重要作用。亚洲大陆的矿产种类最为丰富,在全球80多种广泛使用的矿产中,亚洲大陆至少有38种矿产储量,占全球总储量的30%以上。亚洲大陆经历了三个主要的构造演化和成矿阶段:前寒武纪、古生代和中生代至新生代。该大陆矿产资源丰富,可划分为7个一级成矿带(成矿域)、18个二级成矿带(成矿省)、61个三级成矿带(成矿带)和9个主要成矿系列。亚洲大陆在各大洲中表现出最显著的成矿专门化。具体而言,亚洲大陆花岗岩带具有明显的锡、稀有金属和斑岩型铜、金、钼矿床成矿专一性。其镁铁质岩带和蛇绿岩带表现出明显的红土型镍矿床和岩浆型铬铁矿床的成矿专门性,其中新生代玄武岩带表现出明显的红土型铝土矿床的成矿专门性。形成了东南亚锡成矿带、青藏高原稀有金属成矿带、特提斯斑岩铜金钼成矿带、环太平洋斑岩铜金钼成矿带、东南亚红土铝土矿成矿带、德干高原红土铝土矿成矿带、印度德干高原红土铝土矿成矿带、东南亚红土镍成矿带等大型成矿带。特提斯岩浆型铬铁矿成矿带是亚洲大陆重要的成矿带。未来亚洲地区的矿产勘查应重点关注古克拉通的前寒武纪成矿作用、中亚-蒙古造山带的古生代成矿作用以及特提斯和环太平洋活动带的中生代至新生代成矿作用。亚洲矿业不仅支撑着亚洲经济增长,也带动着世界经济发展和工业化进程,为世界经济发展作出了重要贡献。亚洲是各大洲矿产产值最高、矿产年产量最大、矿产品贸易额最大的地区,已成为全球矿产品贸易中心和矿业经济中心。中国是世界上少有的矿产种类最丰富的国家之一,矿业支撑和带动了亚洲乃至世界的经济发展和工业化。2022年,中国28种矿产品产量居世界首位,是世界第一大矿产品生产国。此外,中国是世界上矿产年产值最高、矿产品贸易额最大的国家。因此,中国对全球矿产品的需求影响着全球矿产品供需格局和世界经济形势。
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引用次数: 0
Ground motion, liquefaction and hazard analysis at the Palu site during the 2018 Indonesian great earthquake (Mw 7.5) 2018年印度尼西亚7.5级大地震期间帕卢地区的地面运动、液化和危害分析
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-01 Epub Date: 2026-02-20 DOI: 10.31035/cg2024067
Lindung Zalbuin Mase , Weeradetch Tanapalungkorn , Suched Likitlersuang , Kyohei Ueda , Tetsuo Tobita
The research findings on the ground motion and liquefaction potential analyses during the 2018 Great Indonesia Earthquake (Mw 7.5) are significant and crucial. The earthquake triggered soil-structure damage due to liquefaction. This study, which thoroughly investigated four sites at Palu, was conducted by performing a comprehensive ground motion parameter analysis. The ground motion characteristics were presented and justified, particularly for the most impacted direction. Ground motion predictions were analysed to define the spectral accelerations, and matching spectral accelerations were conducted to produce ground motions for each site. Non-linear seismic ground response analysis based on the hyperbolic model of pressure pressure-dependent was performed to investigate cyclic soil behaviour. The results revealed that ground motion is crucial in significant soil damage, and the earthquake energy could trigger deep liquefaction. As the most significant ground motion, the vertical ground motion is essential in determining deep liquefaction. The discussion on the impact of liquefaction based on the results of the numerical analysis is presented. Significant ground motion with a longer duration could have a substantial impact on deep liquefaction in the study area. These findings depict how the 2018 Indonesia Earthquake (Mw 7.5) triggered a mega-liquefaction in Palu City. The results could enhance the understanding of the importance of seismic hazard assessment. It is recommended that site investigation and soil improvement should be planned to counteract liquefaction damage before construction. This study also suggests conducting seismic hazard assessments for city development to minimise the potential disaster impact in the study area.
2018年印度尼西亚7.5级大地震的地面运动和液化潜力分析研究成果具有重要意义。地震引起了土壤结构的液化破坏。这项研究通过进行全面的地面运动参数分析,对帕卢的四个地点进行了彻底的调查。提出并论证了地面运动特性,特别是受影响最大的方向。对地面运动预测进行分析,以确定频谱加速度,并进行匹配的频谱加速度,以产生每个站点的地面运动。基于压力-压力相关双曲模型进行了非线性地震地面反应分析,研究了土体的循环特性。结果表明,地震动对土体的重大破坏至关重要,地震能量可引发深层液化。垂直地震动作为最重要的地面运动,对确定深层液化至关重要。在数值分析结果的基础上,对液化的影响进行了讨论。持续时间较长的强烈地震动会对研究区深部液化产生重大影响。这些发现描述了2018年印度尼西亚地震(7.5兆瓦)如何引发帕卢市的巨型液化。研究结果可提高人们对地震危险性评价重要性的认识。建议在施工前进行现场调查和土壤改良,以抵消液化破坏。本研究还建议对城市发展进行地震危害评估,以尽量减少研究区域的潜在灾害影响。
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引用次数: 0
Editorial Committee of China Geology 《中国地质》编辑委员会
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-01 Epub Date: 2026-02-20 DOI: 10.1016/S2096-5192(26)00017-0
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引用次数: 0
Phase field model of fracture propagation and pressure evolution induced by fluid injection considering the effect of initial stress field in power generation test project of Gonghe Basin, China 考虑初始应力场影响的共和盆地发电试验工程注液裂缝扩展与压力演化相场模型
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-01 Epub Date: 2026-02-20 DOI: 10.31035/cg2024034
Hong-wei Wang , Hai-dong Wu , He-juan Liu , Yong-bo Tie , Li-sha Hu , Lin-you Zhang , Xian-peng Jin
Hydraulic stimulation technology is widely employed to enhance the permeability of geothermal reservoirs. Nevertheless, accurately predicting hydraulic fracture propagation in complex geological conditions remains challenging, thereby hindering the effective utilization of existing natural fractures. In this study, a phase field model was developed utilizing the finite element method to examine the influence of fluid presence, stress conditions, and natural fractures on the initiation and propagation of hydraulic fractures. The model employs Biot's poroelasticity theory to establish the coupling between the displacement field and the fluid field, while the phase field theory is applied to simulate fracture behavior. The results show that when σx0y0 < 3 or qf < 20 kg/(m3·s), the presence of natural fractures can alter the original propagation direction of hydraulic fractures. Conversely, in the absence of these conditions, the propagation path of natural fractures is predominantly influenced by the initial stress field. Furthermore, based on the analysis of breakdown pressure and damage area, the optimal intersection angle between natural fractures and hydraulic fractures is determined to range from 45° to 60°. Finally, once a dominant channel forms, initiating and propagating hydraulic fractures in other directions becomes increasingly difficult, even in highly fractured areas. This method tackles the challenges of initiating and propagating hydraulic fractures in complex geological conditions, providing a theoretical basis for optimizing Enhanced Geothermal System (EGS) projects.
水力增产技术被广泛应用于提高地热储层渗透率。然而,在复杂的地质条件下,准确预测水力裂缝的扩展仍然是一个挑战,从而阻碍了现有天然裂缝的有效利用。本研究利用有限元方法建立了相场模型,考察了流体存在、应力条件和天然裂缝对水力裂缝起裂和扩展的影响。该模型采用Biot的孔隙弹性理论建立位移场与流体场之间的耦合关系,采用相场理论模拟裂缝行为。结果表明:当σx0/σy0 <; 3或qf <; 20 kg/(m3·s)时,天然裂缝的存在会改变水力裂缝原有的扩展方向;相反,在没有这些条件的情况下,天然裂缝的扩展路径主要受初始应力场的影响。在分析破裂压力和破坏面积的基础上,确定天然裂缝与水力裂缝的最佳相交角为45°~ 60°。最后,一旦优势通道形成,在其他方向上启动和扩展水力裂缝变得越来越困难,即使在高度压裂的地区也是如此。该方法解决了复杂地质条件下水力裂缝的启动和扩展问题,为优化增强型地热系统(EGS)项目提供了理论基础。
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引用次数: 0
Reservoir fluid type identification method based on deep learning: A case study of the Chang 1 Formation in the Jiyuan oilfield of the Ordos basin, China 基于深度学习的储层流体类型识别方法——以鄂尔多斯盆地姬塬油田长1组为例
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-01 Epub Date: 2026-02-20 DOI: 10.31035/cg2025010
Wen-bo Li , Xiao-ye Wang , Lei He , Zhen-kai Zhang , Zeng-lin Hong , Ling-yi Liu , Dong-tao Li
With the efficient and intelligent development of computer-based big data processing, applying machine learning methods to the processing and interpretation of logging data in the field of geophysical well logging has broad potential for improving production efficiency. Currently, the Jiyuan Oilfield in the Ordos Basin relies mainly on manual reprocessing and interpretation of old well logging data to identify different fluid types in low-contrast reservoirs, guiding subsequent production work. This study uses well logging data from the Chang 1 reservoir, partitioning the dataset based on individual wells for model training and testing. A deep learning model for intelligent reservoir fluid identification was constructed by incorporating the focal loss function. Comparative validations with five other models, including logistic regression (LR), naive Bayes (NB), gradient boosting decision trees (GBDT), random forest (RF), and support vector machine (SVM), show that this model demonstrates superior identification performance and significantly improves the accuracy of identifying oil-bearing fluids. Mutual information analysis reveals the model's differential dependency on various logging parameters for reservoir fluid identification. This model provides important references and a basis for conducting regional studies and revisiting old wells, demonstrating practical value that can be widely applied.
随着计算机大数据处理的高效、智能化发展,将机器学习方法应用于物探测井领域的测井数据处理与解释,在提高生产效率方面具有广阔的潜力。目前,鄂尔多斯盆地济源油田主要依靠人工对老测井资料进行再处理和解释,识别低对比储层的不同流体类型,指导后续的生产工作。本研究使用长1油藏的测井数据,根据单井划分数据集进行模型训练和测试。引入焦点损失函数,建立了储层流体智能识别的深度学习模型。与逻辑回归(LR)、朴素贝叶斯(NB)、梯度增强决策树(GBDT)、随机森林(RF)和支持向量机(SVM)等5种模型的对比验证表明,该模型具有较好的识别性能,显著提高了含油流体的识别精度。互信息分析揭示了该模型对不同测井参数的差异性依赖。该模型为开展区域研究和老井回访提供了重要参考和依据,具有广泛应用的实用价值。
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引用次数: 0
Enhancing rock slope stability prediction using random forest machine learning: A case study 利用随机森林机器学习增强岩质边坡稳定性预测:一个案例研究
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-25 Epub Date: 2025-11-18 DOI: 10.31035/cg2023102
Afiqah Ismail , Ahmad Safuan A Rashid , Ali Dehghanbanadaki , Rafiuddin Hakim Roslan , Mohd Firdaus Md Dan @ Azlan , Abd Wahid Rasib , Radzuan Saari , Mushairry Mustaffar , Azman Kassim , Rini Asnida Abdullah , Khairul Hazman Padil , Norbazlan Mohd Yusof , Norisam Abd Rahaman
The prediction of slope stability is a complex nonlinear problem. This paper proposes a new method based on the random forest (RF) algorithm to study the rocky slopes stability. Taking the Bukit Merah, Perak and Twin Peak (Kuala Lumpur) as the study area, the slope characteristics of geometrical parameters are obtained from a multidisciplinary approach (consisting of geological, geotechnical, and remote sensing analyses). 18 factors, including rock strength, rock quality designation (RQD), joint spacing, continuity, openness, roughness, filling, weathering, water seepage, temperature, vegetation index, water index, and orientation, are selected to construct model input variables while the factor of safety (FOS) functions as an output. The area under the curve (AUC) value of the receiver operating characteristic (ROC) curve is obtained with precision and accuracy and used to analyse the predictive model ability. With a large training set and predicted parameters, an area under the ROC curve (the AUC) of 0.95 is achieved. A precision score of 0.88 is obtained, indicating that the model has a low false positive rate and correctly identifies a substantial number of true positives. The findings emphasise the importance of using a variety of terrain characteristics and different approaches to characterise the rock slope.
边坡稳定性预测是一个复杂的非线性问题。本文提出了一种基于随机森林算法的岩质边坡稳定性研究新方法。以武吉美拉,霹雳州和双峰(吉隆坡)为研究区域,通过多学科方法(包括地质,岩土工程和遥感分析)获得几何参数的边坡特征。选取岩石强度、岩石质量标识(RQD)、节理间距、连续性、开放性、粗糙度、充填、风化、渗水、温度、植被指数、水分指数、方位等18个因素作为模型输入变量,安全系数(FOS)作为输出。精确准确地获得受试者工作特征曲线的曲线下面积(AUC)值,并用于分析预测模型的能力。在较大的训练集和预测参数下,实现了0.95的ROC曲线下面积(AUC)。得到的精度分数为0.88,表明该模型具有较低的假阳性率,并且正确识别了大量的真阳性。研究结果强调了使用各种地形特征和不同方法来表征岩石边坡的重要性。
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引用次数: 0
Lishiite, (Ca2□)Sr3(CO3)5, a new burbankite mineral from carbonatite-syenite complex in Shaxiongdong, Hubei, China 李氏石,(Ca2□)Sr3(CO3)5,一种来自湖北沙雄洞碳酸岩-正长岩杂岩的新伯班特矿物
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-25 Epub Date: 2025-11-18 DOI: 10.31035/cg2025163
Jie Dai , Xiao-dong Pan , Tong Wang , Guo-wu Li , Guan Wang , Shang-ke Xie , Jing Ren , Kun-yang Wang , Ting Li , Tao Wang , Jia-le He , Jin-sha Xu , Gan-fu Shen
Lishiite, (Ca2□)Sr3(CO3)5, is a new mineral species from Shaxiongdong, Hubei Province, China. It mainly occours as conchoidal crystals and with combination of hexagonal prism and pyramid and is associated with calcite, K-feldspar, albite, aegirine, apatite, and ancylite-(Ce)(?) and strontianite etc. Lishiite is brittle with conchiform fracture and has a Mohs hardness of approximately 4 and none cleavages were observed. The Vickers microhardness (VHN10) is 197.42 kg/mm2 (range: 166.88 kg/mm2 to 214.58 kg/mm2), and the calculated density of lishiite is 3.696 g/cm3 . Hand specimen of lishiite are yellow-brown. The empirical chemical formula of the lishiite is A(Ca1.18Sr0.25Na0.191.38)Σ3.00 B[Sr2.17(Ce0.42La0.24Nd0.09Eu0.01)Σ0.76 Ba0.07]Σ3.00 (C5.05O15). As a member of the burbankite group, the general formula of lishiite follows the general formula A3B3(CO3)5, where A=Na, Ca, or and B=Sr, Ba, REE, or Ca. Its crystal structure is hexagonal (space group P63mc) with unit cell parameters a=10.4898(5) Å, c=6.4167(5) Å, and V=611.47(6) Å3, characterized by layers of AO8 and BO10 polyhedra connected to [CO3]3− groups. The discovery of lishiite provides new insights into the evolutionary history of rare earth element (REE) carbonate deposit formation.
石石(Ca2□)Sr3(CO3)5是湖北沙雄洞的一种新矿物。它主要以贝壳状晶体形式出现,并以六棱柱状和棱锥状组合存在,伴生有方解石、钾长石、钠长石、绿柱石、磷灰石、铁云母(Ce)(?)和菱锰矿等。理石易碎,呈螺形断口,莫氏硬度约为4,无解理。维氏显微硬度(VHN10)为197.42 kg/mm2(范围:166.88 kg/mm2 ~ 214.58 kg/mm2),计算得到的利氏石密度为3.696 g/cm3。石纹石的手部标本呈黄褐色。历石的经验化学式为A(Ca1.18Sr0.25Na0.19□1.38)Σ3.00 B[Sr2.17(Ce0.42La0.24Nd0.09Eu0.01)Σ0.76 Ba0.07]Σ3.00 (C5.05O15)。石石属burbankite族,通式为A3B3(CO3)5,其中a= Na、Ca、or, B=Sr、Ba、REE、Ca。石石的晶体结构为六边形(空间群P63mc),晶胞参数a=10.4898(5) Å, c=6.4167(5) Å, V=611.47(6) Å3,以AO8和BO10多面体层连接[CO3]3−基团为特征。理石的发现为研究稀土碳酸盐矿床形成的演化历史提供了新的思路。
{"title":"Lishiite, (Ca2□)Sr3(CO3)5, a new burbankite mineral from carbonatite-syenite complex in Shaxiongdong, Hubei, China","authors":"Jie Dai ,&nbsp;Xiao-dong Pan ,&nbsp;Tong Wang ,&nbsp;Guo-wu Li ,&nbsp;Guan Wang ,&nbsp;Shang-ke Xie ,&nbsp;Jing Ren ,&nbsp;Kun-yang Wang ,&nbsp;Ting Li ,&nbsp;Tao Wang ,&nbsp;Jia-le He ,&nbsp;Jin-sha Xu ,&nbsp;Gan-fu Shen","doi":"10.31035/cg2025163","DOIUrl":"10.31035/cg2025163","url":null,"abstract":"<div><div>Lishiite, (Ca<sub>2</sub>□)Sr<sub>3</sub>(CO<sub>3</sub>)<sub>5</sub>, is a new mineral species from Shaxiongdong, Hubei Province, China. It mainly occours as conchoidal crystals and with combination of hexagonal prism and pyramid and is associated with calcite, K-feldspar, albite, aegirine, apatite, and ancylite-(Ce)(?) and strontianite etc. Lishiite is brittle with conchiform fracture and has a Mohs hardness of approximately 4 and none cleavages were observed. The Vickers microhardness (VHN10) is 197.42 kg/mm<sup>2</sup> (range: 166.88 kg/mm<sup>2</sup> to 214.58 kg/mm<sup>2</sup>), and the calculated density of lishiite is 3.696 g/cm<sup>3 .</sup> Hand specimen of lishiite are yellow-brown. The empirical chemical formula of the lishiite is <sup><em>A</em></sup>(Ca<sub>1.18</sub>Sr<sub>0.25</sub>Na<sub>0.19</sub>□<sub>1.38</sub>)<sub>Σ3.00</sub> <sup><em>B</em></sup>[Sr<sub>2.17</sub>(Ce<sub>0.42</sub>La<sub>0.24</sub>Nd<sub>0.09</sub>Eu<sub>0.01</sub>)<sub>Σ0.76</sub> Ba<sub>0.07</sub>]<sub>Σ3.00</sub> (C<sub>5.05</sub>O<sub>15</sub>). As a member of the burbankite group, the general formula of lishiite follows the general formula <em>A</em><sub>3</sub><em>B</em><sub>3</sub>(CO<sub>3</sub>)<sub>5</sub>, where <em>A</em>=Na, Ca, or and <em>B</em>=Sr, Ba, <em>REE</em>, or Ca. Its crystal structure is hexagonal (space group <em>P</em>6<sub>3</sub><em>mc</em>) with unit cell parameters a=10.4898(5) Å, c=6.4167(5) Å, and V=611.47(6) Å<sup>3</sup>, characterized by layers of <em>A</em>O<sub>8</sub> and <em>B</em>O<sub>10</sub> polyhedra connected to [CO<sub>3</sub>]<sup>3−</sup> groups. The discovery of lishiite provides new insights into the evolutionary history of rare earth element (REE) carbonate deposit formation.</div></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"8 4","pages":"Pages 797-805"},"PeriodicalIF":4.7,"publicationDate":"2025-11-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145537179","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Characteristics of strike-slip fault-related fractures and their controls on reservoir in Halahatang area, northern Tarim Basin 塔北哈拉哈塘地区走滑断裂相关裂缝特征及其对储层的控制作用
IF 4.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2025-11-25 Epub Date: 2025-11-18 DOI: 10.31035/cg2023085
Xiao-xu Liu , Guang-hui Wu , Li-xin Chen , Bing-shan Ma , Zhou Su , Bo Yang , Xia Wang , Bin Zhao
The strike-slip fault system in the central Tarim Craton controls a complex petroleum system with estimated reserves exceeding 1×109 t, the fault-related fractures are important for hydrocarbon accumulation. In this paper, the basic parameters such as density and width of fractures are counted and classified, and the effects of fractures on reservoirs are analyzed. The results show that: (1) Structural fractures and stylolite were widely developed in Halahatang area and experienced at least three stages of activity based on the infilling materials and crosscutting relationship. (2) Fracture density, width, aperture, and dip angle vary in different wells, but the relationship between the above parameters and the distance to the fault core indicates the fracture differences in the fault damage zone and further provides a method to divide the inner units in the fault damage zone. In addition, oil and gas wells with high production mainly concentrate in the inner unit. (3) The infilling materials and degree of fractures vary. Fractures formed in the early stage are more filled and less open, while the fractures formed in the late stage are relatively less filled and more open. (4) Fractures improve porosity to a certain extent but greatly increase permeability, especially in the inner zone of fault damage zone with large quantity, multiple inclinations, less filling and large width. These features contribute to the formation of a higher-quality reservoir, further improving oil and gas production. This paper provides a quantitative characterization method for the study of strike-slip fault-related fracture-caved reservoirs, and points out that fault damage zone, especially the inner zone of the fault damage zone, is the potential goal for oil and gas exploration.
塔中克拉通走滑断裂系统控制着一个复杂的含油气系统,估计储量超过1×109 t,断层相关裂缝对油气成藏具有重要意义。本文对裂缝密度、裂缝宽度等基本参数进行了统计和分类,分析了裂缝对储层的影响。结果表明:(1)从充填物和横切关系来看,哈拉哈塘地区构造裂缝和柱化岩广泛发育,经历了至少3期活动;(2)不同井的裂缝密度、裂缝宽度、裂缝孔径和裂缝倾角各不相同,但上述参数与断层岩心距离的关系表明了断层损伤带的裂缝差异,为断层损伤带内部单元的划分提供了一种方法。此外,高产油气井主要集中在内单元。(3)充填材料和破裂程度不同。早期形成的裂缝充填程度较高,开放程度较低,而后期形成的裂缝充填程度相对较低,开放程度较高。(4)裂缝在一定程度上改善了孔隙度,但大大增加了渗透率,特别是在数量多、倾角多、充填少、宽度大的断层破坏带内带。这些特征有助于形成更高质量的储层,进一步提高油气产量。本文为走滑断层相关缝洞型储层的研究提供了定量表征方法,并指出断层破坏带特别是断层破坏带内带是油气勘探的潜在目标。
{"title":"Characteristics of strike-slip fault-related fractures and their controls on reservoir in Halahatang area, northern Tarim Basin","authors":"Xiao-xu Liu ,&nbsp;Guang-hui Wu ,&nbsp;Li-xin Chen ,&nbsp;Bing-shan Ma ,&nbsp;Zhou Su ,&nbsp;Bo Yang ,&nbsp;Xia Wang ,&nbsp;Bin Zhao","doi":"10.31035/cg2023085","DOIUrl":"10.31035/cg2023085","url":null,"abstract":"<div><div>The strike-slip fault system in the central Tarim Craton controls a complex petroleum system with estimated reserves exceeding 1×10<sup>9</sup> t, the fault-related fractures are important for hydrocarbon accumulation. In this paper, the basic parameters such as density and width of fractures are counted and classified, and the effects of fractures on reservoirs are analyzed. The results show that: (1) Structural fractures and stylolite were widely developed in Halahatang area and experienced at least three stages of activity based on the infilling materials and crosscutting relationship. (2) Fracture density, width, aperture, and dip angle vary in different wells, but the relationship between the above parameters and the distance to the fault core indicates the fracture differences in the fault damage zone and further provides a method to divide the inner units in the fault damage zone. In addition, oil and gas wells with high production mainly concentrate in the inner unit. (3) The infilling materials and degree of fractures vary. Fractures formed in the early stage are more filled and less open, while the fractures formed in the late stage are relatively less filled and more open. (4) Fractures improve porosity to a certain extent but greatly increase permeability, especially in the inner zone of fault damage zone with large quantity, multiple inclinations, less filling and large width. These features contribute to the formation of a higher-quality reservoir, further improving oil and gas production. This paper provides a quantitative characterization method for the study of strike-slip fault-related fracture-caved reservoirs, and points out that fault damage zone, especially the inner zone of the fault damage zone, is the potential goal for oil and gas exploration.</div></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"8 4","pages":"Pages 740-753"},"PeriodicalIF":4.7,"publicationDate":"2025-11-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145537195","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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China Geology
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