Geological Journal最新文献

{"title":"Magnetostratigraphy and rock magnetic studies on the Cretaceous-Paleogene transition strata along the Um Sohryngkew River, Therriaghat, Meghalaya, India","authors":"Debarati Nag,&nbsp;Satish J. Sangode,&nbsp;Sarvendra P. Singh,&nbsp;Prem R. Uddandam,&nbsp;Adrita Choudhuri,&nbsp;Binita Phartiyal,&nbsp;Vandana Prasad","doi":"10.1002/gj.5046","DOIUrl":"10.1002/gj.5046","url":null,"abstract":"<p>A combination of magnetic polarity and rock magnetic analysis on the well-documented section of the Um Sohryngkew River (USR) in the south Shillong Plateau, NE India, produced a sharp reversal marking the C29r-C29n geomagnetic polarity transition at approximately 65.688 Ma. The rock magnetic studies indicate ferrimagnetic dominant mineralogy with abundance of SSD grains, with an anomalous peak in susceptibility coinciding with Ir-rich limonitic layer. The magnetic reversal occurs precisely 61 m above the Ir-rich distinct in situ limonitic layer, indicating that the C29r-C29n geomagnetic reversal post-dates the widely accepted Ir-anomaly based K-Pg boundary by approximately 355 Ka. Furthermore, the rock magnetic studies indicate its frequency dependence coinciding with the Ir-rich limonitic layer suggesting a possible dust/aerosol source, while akaganéite is reported from the interval approximately 1 m below peak susceptibility, indicating signature of Deccan volcanism. This study infers the completeness of the USR section with a high rate of sedimentation of approximately 17 cm/ka among the marine K-Pg boundary sections in the world.</p>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"59 11","pages":"3048-3067"},"PeriodicalIF":1.4,"publicationDate":"2024-08-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215388","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Mantle dynamics of the stagnating slab: A case study of Shandong Peninsula and adjacent areas","authors":"Kailun Ba,&nbsp;Haimeng Xue,&nbsp;Lin Liu,&nbsp;Jianping Huang,&nbsp;Junhao Qu","doi":"10.1002/gj.5045","DOIUrl":"10.1002/gj.5045","url":null,"abstract":"<p>The Shandong Peninsula is located in the eastern part of the North China Craton (NCC). Influenced by the collision between the North and South China blocks and the subduction of the Pacific Plate, the tectonic evolution process is highly complex. Previous studies have proposed that the thick cratonic root beneath the eastern NCC has been destructed. To better understand the relationship between the craton reactivation and the deep subduction, more constraints on the topography variations of the mantle transition zone (MTZ) discontinuities are required. In this study, we stacked 9073 P-to-S receiver functions calculated from 129 broadband seismic stations to image the depth variations of the MTZ discontinuities beneath the Shandong Peninsula and its adjacent area. To decrease the influence of velocity anomaly above the MTZ discontinuities, we converted the apparent depths into corrected depth using regional and global 3D velocity models. The apparent depth of the 410-km discontinuity exhibits a depression of approximately 6 km, which normalizes after velocity correction. This implies the existence of the low-velocity anomaly in the upper mantle, possibly caused by slab dehydration and water infiltration into the upper mantle. The significant depression of the 660-km discontinuity indicated the presence of the cold Pacific slab stagnating at the base of the MTZ. The gradual westward depression of the 660-km discontinuity by 50 km could provide evidence for the sinking of the western margin of the flat-lying subducting Pacific slab in the MTZ beneath the Shandong Peninsula.</p>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"60 2","pages":"311-319"},"PeriodicalIF":1.4,"publicationDate":"2024-08-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215382","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Reliability-based state parameter liquefaction probability prediction using soft computing techniques","authors":"Kishan Kumar,&nbsp;Pijush Samui,&nbsp;S. S. Choudhary","doi":"10.1002/gj.5049","DOIUrl":"10.1002/gj.5049","url":null,"abstract":"<p>The state parameter (<i>ѱ</i>) accounts for both relative density and effective stress, which influence the cyclic stress or liquefaction characteristic of the soil significantly. This study presents a <i>ѱ-</i>based probabilistic liquefaction evaluation method using six soft computing (SC) techniques. The liquefaction probability of failure (<i>P</i>_<i>L</i>) 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 <i>P</i>_<i>L</i>. 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 <i>P</i>_<i>L</i> 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 <i>P</i>_<i>L</i>. The results of the sensitivity analysis reveal the magnitude of earthquake (<i>M</i>_<i>w</i>) 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.</p>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"59 9","pages":"2638-2654"},"PeriodicalIF":1.4,"publicationDate":"2024-08-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215386","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Analysis of Carboniferous-Permian coal-accumulating environment and coalbed methane enrichment in the southern Qinshui Basin","authors":"Xiaojun Zhang","doi":"10.1002/gj.5050","DOIUrl":"10.1002/gj.5050","url":null,"abstract":"<p>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.</p>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"59 11","pages":"3080-3091"},"PeriodicalIF":1.4,"publicationDate":"2024-08-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215384","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Late Mesozoic ductile deformation and exhumation along the Shangdan suture zone in the Qinling Orogenic Belt, China","authors":"Le Zhang,&nbsp;Wei Li,&nbsp;Dazhi Jiang,&nbsp;Li Liang,&nbsp;Liuqing Jiang,&nbsp;Chao Wang,&nbsp;Zhenwei Feng,&nbsp;Zhihao Ma,&nbsp;Falak Sheir","doi":"10.1002/gj.5037","DOIUrl":"10.1002/gj.5037","url":null,"abstract":"<p>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.</p>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"59 11","pages":"2941-2966"},"PeriodicalIF":1.4,"publicationDate":"2024-08-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215387","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Renewable energy, financial globalization and load capacity factor in the US: Ecological neutrality in the context of natural resources","authors":"Saifullahi Sani Ibrahim,&nbsp;Ahmed Samour,&nbsp;Hamza Almassri,&nbsp;Joanna Kurowska-Pysz","doi":"10.1002/gj.5043","DOIUrl":"10.1002/gj.5043","url":null,"abstract":"<p>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.</p>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"59 11","pages":"3017-3032"},"PeriodicalIF":1.4,"publicationDate":"2024-08-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215390","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Geological characteristics and ore-forming conditions of the Tasikmadu porphyry Cu–Au prospect in Trenggalek, East Java, Indonesia","authors":"Arifudin Idrus,&nbsp;Genki Kaneko,&nbsp;Ryohei Takahashi,&nbsp;Finlan Adhitya Aldan,&nbsp;Trifatama Rahmalia,&nbsp;Hinako Sato","doi":"10.1002/gj.5042","DOIUrl":"10.1002/gj.5042","url":null,"abstract":"<p>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 δ³⁴S_CDT 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.</p>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"59 11","pages":"2990-3016"},"PeriodicalIF":1.4,"publicationDate":"2024-08-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215391","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The superposition of Cretaceous mineralization events leading to the formation of the large Baiyinnuoer Pb–Zn deposit in NE China","authors":"Ruiliang Wang,&nbsp;Jie Wang,&nbsp;Yuling Zhao,&nbsp;Qingdong Zeng,&nbsp;Xiaowei Wang,&nbsp;Jinzhong Yang,&nbsp;Yunpeng Guo,&nbsp;Bing Yu,&nbsp;Jinjian Wu","doi":"10.1002/gj.5039","DOIUrl":"10.1002/gj.5039","url":null,"abstract":"<p>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.</p>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"59 11","pages":"2967-2989"},"PeriodicalIF":1.4,"publicationDate":"2024-08-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215389","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Design and construction of tunnels and tunnelling: Understanding the importance of geological conditions, landslide susceptibility and risk assessment","authors":"Wengang Zhang,&nbsp;Ian Somerville,&nbsp;Gustavo Paneiro,&nbsp;Xingzhong Nong,&nbsp;Marcin Chwala,&nbsp;Wenyu Yang","doi":"10.1002/gj.5041","DOIUrl":"10.1002/gj.5041","url":null,"abstract":"<p>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.</p>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"59 9","pages":"2365-2370"},"PeriodicalIF":1.4,"publicationDate":"2024-08-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215420","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The effect of soil conditions on the dynamic response of shield tunnels under train-induced vibration loads","authors":"Wenbo Yang,&nbsp;Liangliang Zhao,&nbsp;Chaofan Yao,&nbsp;Qixiang Yan,&nbsp;Kun Qian,&nbsp;Jun Yang,&nbsp;Wengang Zhang","doi":"10.1002/gj.5040","DOIUrl":"10.1002/gj.5040","url":null,"abstract":"<p>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.</p>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"59 9","pages":"2690-2701"},"PeriodicalIF":1.4,"publicationDate":"2024-08-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142215392","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}