Results for 'Renate Pore'

589 found
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  1. Mind Matters.Ernest Le Pore & Barry Loewer - 1987 - Journal of Philosophy 84 (11):630 - 642.
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  2.  31
    Pronouns and Quantifier-Scope in English.Ernest Pore & James Garson - 1983 - Journal of Philosophical Logic 12 (3):327 - 358.
    This paper is truly a joint effort and it could not have been written without the contribution of both authors. Garson, though, deserves credit (or blame) for first seeing the need for two kinds of quantifier scope, and also for devising essentials of the positive theory.
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  3.  28
    Transcranial Direct Current Stimulation of Prefrontal Cortex: An Event-Related Potential and Proton Magnetic Resonance Spectroscopy Study.Knechtel Lilly, Schall Ulrich, Cooper Gavin, Jolly Todd, Stanwell Peter, Ramadan Saalladah & Thienel Renate - 2015 - Frontiers in Human Neuroscience 9.
  4.  24
    Variability in Inter-Trial Coherence Predicts Variability in Cognitive Control Efficiency.Wong Aaron, Cooper Patrick, Thienel Renate, Michie Patricia & Karayanidis Frini - 2015 - Frontiers in Human Neuroscience 9.
  5.  12
    Mismatch Negativity in Autism Spectrum Disorder.Schall Ulrich, Weismueller Benjamin, Thienel Renate, Youlden Anne-Marie & Fulham Ross - 2015 - Frontiers in Human Neuroscience 9.
  6.  8
    Individual Differences in Salience and Executive-Control Networks.Rennie Jaime, Cooper Patrick, Thienel Renate & Karayanidis Frini - 2015 - Frontiers in Human Neuroscience 9.
  7.  8
    Dissociable Frontoparietal Oscillatory Networks For Proactive and Reactive Control Characterised Using Complex Network Analyses.Cooper Patrick, Wong Aaron, Thienel Renate, Michie Patricia & Karayanidis Frini - 2015 - Frontiers in Human Neuroscience 9.
  8.  9
    The Concept of Meaning and its Role in Understanding Language.Ernest Le Pore - 1983 - Dialectica 37 (2):133-139.
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  9. The Study of Organizations.Mayntz Renate - 1964 - Social Research 32:239-255.
     
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  10.  8
    Translocation Through the Nuclear Pore: Kaps Pave the Way.Reiner Peters - 2009 - Bioessays 31 (4):466-477.
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  11.  10
    Two-Parameter Prestack Seismic Inversion of Porosity and Pore Structure Parameter of Fractured Carbonate Reservoirs: Part 1 — Methods.Tingting Zhang & Yuefeng Sun - 2018 - Interpretation: SEG 6 (4):SM1-SM8.
    Fractured zones in deeply buried carbonate hills are important because they often have better permeability resulting in prolific production than similar low-porosity rocks. Nevertheless, their detection poses great challenge to conventional seismic inversion methods because they are mostly low in acoustic impedance and bulk modulus, hardly distinguishable from high-porosity zones or mudstones. A proxy parameter of pore structure defined in a rock-physics model, the so-called Sun model, has been used for delineating fractured zones in which the pore structure (...)
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  12.  5
    Stratigraphic and Lithofacies Control on Pore Characteristics of Mississippian Limestone and Chert Reservoirs of North-Central Oklahoma.Fnu Suriamin & Matthew J. Pranter - 2018 - Interpretation: SEG 6 (4):T1001-T1022.
    We have determined how stratigraphy and lithofacies control pore structures in the Mississippian limestone and chert reservoir of north-central Oklahoma. There are 17 lithofacies and 29 high-frequency cycles documented in the Mississippian interval of this study. The high-frequency cycles have thicknesses ranging from 0.3 to 30.5 m and are mainly asymmetric regressive phases. The pore characteristics, measured through digital-image analysis of thin-sections photomicrographs, exhibit unique correlations with core porosity, permeability, and lithofacies within a sequence-stratigraphic framework. There are five (...)
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  13.  2
    Stratigraphic and Lithofacies Control on Pore Characteristics of Mississippian Limestone and Chert Reservoirs of North-Central Oklahoma.Fnu Suriamin & Matthew J. Pranter - 2018 - Interpretation 6 (4):T1001-T1022.
    We have determined how stratigraphy and lithofacies control pore structures in the Mississippian limestone and chert reservoir of north-central Oklahoma. There are 17 lithofacies and 29 high-frequency cycles documented in the Mississippian interval of this study. The high-frequency cycles have thicknesses ranging from 0.3 to 30.5 m and are mainly asymmetric regressive phases. The pore characteristics, measured through digital-image analysis of thin-sections photomicrographs, exhibit unique correlations with core porosity, permeability, and lithofacies within a sequence-stratigraphic framework. There are five (...)
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  14.  4
    The Whole-Aperture Pore-Structure Characteristics of Marine-Continental Transitional Shale Facies of the Taiyuan and Shanxi Formations in the Qinshui Basin, North China.Jiyuan Wang & Shaobin Guo - 2019 - Interpretation 7 (2):T547-T563.
    To systematically study the whole-aperture pore-structure characteristics of the marine-continental transitional shale facies in the Upper Palaeozoic Taiyuan and Shanxi Formations of the Qinshui Basin, we have collected a total of 11 samples for high-pressure mercury intrusion, low-pressure gas adsorption, nuclear magnetic resonance, and field-emission scanning electron microscopy with argon-ion polishing experiments to determine the pore morphology and distribution characteristics of shale samples in detail and to perform quantitative analyses. Then compared the pore-development characteristics of the Taiyuan (...)
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  15.  15
    Two-Parameter Prestack Seismic Inversion of Porosity and Pore-Structure Parameter of Fractured Carbonate Reservoirs: Part 2 — Applications.Tingting Zhang, Ruifeng Zhang, Jianzhang Tian, Lifei Lu, Fengqi Qin, Xianzeng Zhao & Yuefeng Sun - 2018 - Interpretation: SEG 6 (4):SM9-SM17.
    Fractures and fracture-related dissolution pores, as well as cavities, molds, and vugs, provide the major conduit and/or storage space for hydrocarbons in the deeply buried carbonate hill of Hexiwu field, Bohai Bay Basin. The fractured reservoir generally has lower porosity but better permeability than moldic/vuggy reservoir, and it consists of the major part of the buried-hill slope and buried-hill internal reservoirs. The conventional method of characterizing carbonate reservoirs, however, often mixes these two types of reservoirs together because they both have (...)
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  16.  13
    Pore-Throat Structures and Their Control of Terrestrial Lacustrine Tight Reservoir Quality: The Permian Lucaogou Formation, Jimsar Sag, Northwestern China.Ke Ma, Jiagen Hou, Lin Yan & Fuli Chen - 2018 - Interpretation: SEG 6 (4):T889-T906.
    Understanding the structure of the pore throat is an important task for tight reservoir development. The common methods of studying the pore-throat structure include pressure-controlled mercury injection, rate-controlled mercury injection, X-ray computer tomography, and scanning electron microscopy. We have used those four methods to understand the pore-throat structures of three main lithologies in the Lucaogou Formation, Jimsar Sag, China. The PMI results revealed that the pore-throat size of all of the lithologies ranges from 0.013 to [Formula: (...)
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  17.  9
    Two-Parameter Prestack Seismic Inversion of Porosity and Pore Structure Parameter of Fractured Carbonate Reservoirs: Part 1 — Methods.Tingting Zhang & Yuefeng Sun - 2018 - Interpretation 6 (4):SM1-SM8.
    Fractured zones in deeply buried carbonate hills are important because they often have better permeability resulting in prolific production than similar low-porosity rocks. Nevertheless, their detection poses great challenge to conventional seismic inversion methods because they are mostly low in acoustic impedance and bulk modulus, hardly distinguishable from high-porosity zones or mudstones. A proxy parameter of pore structure defined in a rock-physics model, the so-called Sun model, has been used for delineating fractured zones in which the pore structure (...)
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  18.  8
    Pore-Throat Structures and Their Control of Terrestrial Lacustrine Tight Reservoir Quality: The Permian Lucaogou Formation, Jimsar Sag, Northwestern China.Ke Ma, Jiagen Hou, Lin Yan & Fuli Chen - 2018 - Interpretation 6 (4):T889-T906.
    Understanding the structure of the pore throat is an important task for tight reservoir development. The common methods of studying the pore-throat structure include pressure-controlled mercury injection, rate-controlled mercury injection, X-ray computer tomography, and scanning electron microscopy. We have used those four methods to understand the pore-throat structures of three main lithologies in the Lucaogou Formation, Jimsar Sag, China. The PMI results revealed that the pore-throat size of all of the lithologies ranges from 0.013 to [Formula: (...)
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  19.  12
    Quantitative Characterization and Characteristic Analysis of Pore Structure of Shale-Gas Reservoir in the Sichuan Basin, China.Huaimin Dong, Jianmeng Sun, Jinjiang Zhu, Zhenzhou Lin, Likai Cui, Weichao Yan & Zhu Xiong - 2019 - Interpretation 7 (4):SJ23-SJ32.
    Quantitative characterization of pore structure in shale can provide basic parameters for evaluation of the shale-gas reservoir quality. However, it is difficult to use conventional methods to accurately and comprehensively characterize the pore structure parameters. We take shale samples from the Longmaxi Formation in the Sichuan Basin as the study object, and we use the high-pressure mercury intrusion, nitrogen adsorption, and carbon dioxide adsorption methods to characterize the whole aperture distribution. We found that the pore size in (...)
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  20.  1
    Near-Salt Perturbations of Stresses and Pore Fluid Pressures and Their Impacts on Wellbore Stability in the Kuqa Depression of the Tarim Basin, China.Cheng Chang, Gang Luo, Mingwen Wang & Yunqiang Sun - 2020 - Interpretation 8 (2):SG33-SG49.
    Salt structures are highly associated with economic hydrocarbon reservoirs. However, drilling a wellbore near or through the salt is usually difficult because the near-salt stresses and pore fluid pressures are largely perturbed due to weaker mechanical strength of salt bodies than their surrounding sediments. We have developed a 2D plane-strain poroelastic finite-element model to simulate stresses and pore pressures in the horizontal-compression salt tectonic system, the Kuqa depression in the Tarim Basin, China, and we use the model results (...)
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  21.  7
    Characteristics and Origin of the Pore Structure of the Lacustrine Tight Oil Reservoir in the Northwestern Jiuquan Basin, China.Chunyan Fan, Xianglu Tang, Yuanyin Zhang, Yan Song, Zhenxue Jiang, Qun Luo & Baiying Li - 2019 - Interpretation 7 (3):T625-T636.
    The pore structure controls the formation processes of tight oil reservoirs. It is meaningful to study the characteristics and origin of the pore structure of the tight oil reservoir. We have analyzed the pore structure of the tight oil reservoir by thin sections, scanning electron microscopy, and mercury intrusion porosimetry. We analyze the origin of the pore structure based on sedimentological, diagenetic, and tectonism processes. The porosity of the tight oil reservoirs is mainly approximately 2%–10%, and (...)
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  22.  2
    An Improved Method to Characterize the Full-Scale Pore System and Dual Pore Model of Tight Sands.Yurui Zhu, Zhengyuan Lu, Mingshi Feng, Jun Wang & Zhipeng Li - 2020 - Interpretation 8 (3):SL9-SL23.
    Tight sands have pore systems with complex structures and widely distributed pore sizes. We have studied the characteristics of these pore systems to better understand their important role in the accumulation and migration mechanisms of oil and gas reservoirs, which may enhance our ability to evaluate reservoir quality and predict reservoir production. To this end, we carried out thin-section analysis, scanning electron microscopy, pressure-controlled porosimetry, and rate-controlled porosimetry to describe the pore systems of a typical tight-sand (...)
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  23.  4
    Investigation of Pore Structure Characteristics of Marine Organic-Rich Shales Using Low-Pressure N2 Adsorption Experiments and Fractal Theory.Difei Zhao, Shuai Yin, Yinghai Guo, Chengyao Ren, Ruyue Wang, Wenlong Dinge & Jingshou Liue - 2019 - Interpretation 7 (3):T671-T685.
    The pore structure and fractal characteristics of the Lower Cambrian marine organic-rich shale in southern China were comprehensively studied using low-pressure [Formula: see text] adsorption and organic geochemical experiments, X-ray diffraction, petrophysical property tests, and scanning electron microscope observations. The results indicate that the total organic carbon content of the study shale varies between 0.45% and 8.50%, with an average value of 3.97%. The adsorption isotherm of the shale samples belongs to type IV, and slit-type pores are the predominant (...)
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  24.  18
    Nietzsche nach dem Ersten Weltkrieg, hg. von Sandro Barbera und Renate Müller-Buck.Renate Reschke & Volker Gerhardt - 2008 - In Renate Reschke & Volker Gerhardt (eds.), Friedrich Nietzsche – Geschichte, Affekte, Medien. Akademie Verlag.
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  25.  13
    Renate LORENZ , Not Now! Now! Chronopolitics, Art & Research.Ophélie Naessens - forthcoming - Rhuthmos.
    Cette recension a déjà paru dans Critique d'art, le 4 novembre 2014. Renate LORENZ, Not Now! Now! Chronopolitics, Art & Research, Berlin, Sternberg Press, 2014, 187 p. Not Now! Now! prolonge les réflexions engagées lors du colloque international éponyme à l'Academy of Fine Arts de Vienne en 2013 qui réunissait théoriciens et artistes autour des chronopolitics. Si la durée, le rythme et l'ordonnancement du temps sont des enjeux majeurs dans la compréhension des évènements - Recensions.
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  26.  1
    Effect of Laminae Development on Pore Structure in the Lower Third Member of the Shahejie Shale, Zhanhua Sag, Eastern China.Tingwei Li, Zhenxue Jiang, Pibo Su, Xi Zhang, Weitao Chen, Xiaoyan Wang, Chuanxiang Ning, Zhi Wang & Zixin Xue - 2020 - Interpretation 8 (1):T103-T114.
    Similar to mineral composition and organic geochemical features, laminae development significantly influences pore structure. Taking the lower third member of the Shahejie Shale, Zhanhua Sag, Eastern China as the research object, we introduced various methods to analyze the influence of laminae development on pore structure, including thin section observations, field emission scanning electron microscopy, gas adsorption, high-pressure mercury injection, nano-computed tomography, quantitative evaluation of minerals by scanning electron microscopy, and spontaneous imbibition. We draw the conclusions that various minerals (...)
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  27.  6
    Recombinational DNA Repair is Regulated by Compartmentalization of DNA Lesions at the Nuclear Pore Complex.Vincent Géli & Michael Lisby - 2015 - Bioessays 37 (12):1287-1292.
    The nuclear pore complex (NPC) is emerging as a center for recruitment of a class of “difficult to repair” lesions such as double‐strand breaks without a repair template and eroded telomeres in telomerase‐deficient cells. In addition to such pathological situations, a recent study by Su and colleagues shows that also physiological threats to genome integrity such as DNA secondary structure‐forming triplet repeat sequences relocalize to the NPC during DNA replication. Mutants that fail to reposition the triplet repeat locus to (...)
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  28. Overburden Characterization with Formation Pore Pressure and Anisotropic Stress Field Estimation in the Athabasca Basin, Canada.Carmen C. Dumitrescu & Draga A. Talinga - 2019 - Interpretation 7 (4):T761-T771.
    One of the challenges encountered during the life cycle of an oil-sand thermal-production reservoir is the prediction of the formation pore pressure and in situ stress regime during the assessment phase of the reservoir development and, more importantly, during the development phase. We have investigated the state of formation pore pressure and stress in the overburden — represented by the Clearwater Formation, Grand Rapids Formation, and Colorado Group — of a preproduction oil-sands reservoir situated in the Athabasca Basin (...)
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  29. Impact of Convective Cooling on Pore Pressure and Stresses Around a Borehole Subjected to a Constant Flux: Implications for Hydraulic Tests in an EGS Reservoir.Zhiqiang Fan, Rishi Parashar & Z. -H. Jin - forthcoming - Interpretation:1-31.
    Hydraulic tests are commonly performed prior to reservoir stimulation to determine the natural permeability of enhanced geothermal system, which typically involves injection of cold water at low rates into the hot target EGS reservoir and measurement of the surface pressure, flow rate, and thermal drawdown simultaneously. Interpretation and analysis of the data collected during a hydraulic test is largely based on fitting type curves generated from analytical solutions. We have formulated a geomechanical model for hydraulic tests in a thermoporoelastic EGS (...)
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  30. Impact of Convective Cooling on Pore Pressure and Stresses Around a Borehole Subjected to a Constant Flux: Implications for Hydraulic Tests in an Enhanced Geothermal System Reservoir.Zhiqiang Fan, Rishi Parashar & Zhi-He Jin - 2020 - Interpretation 8 (2):SG13-SG20.
    Hydraulic tests are commonly performed prior to reservoir stimulation to determine the natural permeability of the enhanced geothermal system, which typically involves injection of cold water at low rates into the hot target EGS reservoir and measurement of the surface pressure, flow rate, and thermal drawdown simultaneously. Interpretation and analysis of the data collected during a hydraulic test are largely based on fitting type curves generated from analytical solutions. We have formulated a geomechanical model for hydraulic tests in a thermoporoelastic (...)
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  31. Pore Structure and Fluid Uptake of the Yeso, Abo, and Cisco Formations in the Permian Basin in Southeast New Mexico, USA.Qinhong Hu, Griffin Mann & Jianhua Zhao - 2019 - Interpretation 7 (4):SK1-SK17.
    There is a need for a petrophysical understanding of producing formations in the Northwest Shelf in southeast New Mexico. Working with six rotary sidewall core samples, we have investigated the utility of mercury injection capillary pressure, contact angle, fluid imbibition, as well as logging analyses to evaluate the characteristics of pore structure and fluid uptake of the Yeso, Abo, and Cisco Formations. Results from MICP tests provide a variety of pore structure data including bulk and particle densities, porosity, (...)
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  32. Renate Bartsch. Adverbialsemantik. Die Konstitution logischsemantischer Repräsentationen von Adverbialkonstruktionen.Ewald Lang & Renate Steinitz - 1976 - Foundations of Language 14:137-151.
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  33. Pore Structure Characteristics and its Effect on Adsorption Capacity of Niutitang Marine Shale in Sangzhi Block, Southern China.Xinghua Wang, Arash Dahi Taleghani & Wenlong Ding - 2019 - Interpretation 7 (4):T843-T856.
    Characteristics of shale pore structures may play an important role in natural gas accumulation and consequently estimating the original gas in place. To determine the pore structure characteristics of Niutitang marine shale in the Sangzhi block, we carried out [Formula: see text] adsorption-desorption, [Formula: see text] adsorption, and methane isothermal adsorption on shale samples to reveal the pore size distribution and its impact on the adsorption capacity. Results indicate that the Niutitang Shale is in stages of maturity (...)
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  34.  28
    Pore Types, Pore-Network Analysis, and Pore Quantification of the Lacustrine Shale-Hydrocarbon System in the Late Triassic Yanchang Formation in the Southeastern Ordos Basin, China.Robert G. Loucks, Stephen C. Ruppel, Xiangzeng Wang, Lucy Ko, Sheng Peng, Tongwei Zhang, Harry D. Rowe & Patrick Smith - 2017 - Interpretation: SEG 5 (2):SF63-SF79.
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  35.  17
    Controls on Pore Types and Pore-Size Distribution in the Upper Triassic Yanchang Formation, Ordos Basin, China: Implications for Pore-Evolution Models of Lacustrine Mudrocks.Lucy T. Ko, Robert G. Loucks, Kitty L. Milliken, Quansheng Liang, Tongwei Zhang, Xun Sun, Paul C. Hackley, Stephen C. Ruppel & Sheng Peng - 2017 - Interpretation: SEG 5 (2):SF127-SF148.
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  36.  31
    An Integrated Approach to Quantify Geologic Controls on Carbonate Pore Types and Permeability, Puguang Gas Field, China.Qifei Huang, Qifeng Dou, Yiwei Jiang, Qingsheng Zhang & Yuefeng Sun - 2017 - Interpretation: SEG 5 (4):T545-T561.
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  37.  25
    Pore Characteristics of Lacustrine Mudstones From the Cretaceous Qingshankou Formation, Songliao Basin.Min Wang, Shuangfang Lu, Wenbiao Huang & Wei Liu - 2017 - Interpretation: SEG 5 (3):T373-T386.
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  38. Philosophie in der Islamischen Welt, Band 1, 8.-10. Jahrhundert (Philosophy in the Islamic World, Volume 1, Eighth to Tenth Centuries) Edited by Ulrich Rudolph, with the Assistance of Renate Würsch (Review). [REVIEW]Tony Street - 2014 - Philosophy East and West 64 (2):515-517.
    Philosophie in der Islamischen Welt, Band 1, 8.-10. Jahrhundert, edited by Ulrich Rudolph, is the first in a series of four volumes devoted to the history of philosophy in the Islamic world from earliest times down to today.1 Part of a larger project that has been under way, in one way or another, for 150 years, this volume marks an epochal moment in the study of Arabic philosophy. Never before in the field has there been a summary exposition so comprehensive, (...)
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  39.  12
    Pore Characteristics and Dominant Controlling Factors of Overmature Shales: A Case Study of the Wangyinpu and Guanyintang Formations in the Jiangxi Xiuwu Basin.Fenglin Gao, Yan Song, Zhuo Li, Zhenxue Jiang, Zhiye Gao, Xinxin Zhang, Lei Chen & Qingxin Liu - 2018 - Interpretation: SEG 6 (2):T393-T412.
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  40.  5
    Single Particle Imaging of mRNAs Crossing the Nuclear Pore: Surfing on the Edge.Alexander F. Palazzo & Mathew Truong - 2016 - Bioessays 38 (8):744-750.
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  41.  15
    Pore Characteristics and Dominant Controlling Factors of Overmature Shales: A Case Study of the Wangyinpu and Guanyintang Formations in the Jiangxi Xiuwu Basin.Fenglin Gao, Yan Song, Zhuo Li, Zhenxue Jiang, Zhiye Gao, Xinxin Zhang, Lei Chen & Qingxin Liu - 2018 - Interpretation 6 (2):T393-T412.
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  42.  12
    Relationship Between Pore Characteristics and Occurrence State of Shale Gas: A Case Study of Lower Silurian Longmaxi Shale in the Upper Yangtze Platform, South China.Lei Chen, Zhenxue Jiang, Keyu Liu, Pengfei Wang, Yu Liu, He Bi, Fenglin Gao, Chen Zhang & Wenming Ji - 2017 - Interpretation: SEG 5 (3):T437-T449.
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  43.  4
    Prestack Simultaneous Inversion to Predict Lithology and Pore Fluid in the Realgrunnen Subgroup of the Goliat Field, Southwestern Barents Sea.Honore Dzekamelive Yenwongfai, Nazmul Haque Mondol, Jan Inge Faleide & Isabelle Lecomte - 2017 - Interpretation: SEG 5 (2):SE75-SE96.
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  44.  20
    Pore-Pressure-Constrained, Rock-Physics-Guided Velocity Model Building Method: Alternate Solution to Mitigate Subsalt Geohazard.Nader Dutta, Bhaskar Deo, Yangjun Liu, Krishna Ramani, Jerry Kapoor & Denes Vigh - 2015 - Interpretation: SEG 3 (1):SE1-SE11.
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  45.  16
    An Integrated Pore-Pressure Model and its Application to Hydrocarbon Exploration: A Case Study From the Mahanadi Basin, East Coast of India.Ajesh John, Ashutosh Kumar, Karthikeyan G. & Pankaj Gupta - 2014 - Interpretation: SEG 2 (1):SB17-SB26.
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  46.  4
    Investigating the Influence of Mineralogy and Pore Shape on the Velocity of Carbonate Rocks: Insights From Extant Global Data Sets.Mark G. Kittridge - 2015 - Interpretation: SEG 3 (1):SA15-SA31.
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  47.  12
    Petrophysical Rock Classification in the Cotton Valley Tight-Gas Sandstone Reservoir with a Clustering Pore-System Orthogonality Matrix.Chicheng Xu & Carlos Torres-Verdín - 2014 - Interpretation: SEG 2 (1):T13-T23.
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  48.  16
    Renate Oswald: Das Ende der Odyssee. Studien zu Strukturen epischen Gestaltens. Pp. 188. Graz: Technische Universität Graz, 1993. Paper, ÖS 110/DM 17. [REVIEW]A. F. Garvie - 1995 - The Classical Review 45 (1):154-154.
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  49.  6
    Interpretation of Hydraulic Rock Types with Resistivity Logs in Tertiary Deepwater Turbidite Reservoirs: Pore-Scale Modeling Verified with Field Observations in the Gulf of Mexico, USA.Chicheng Xu, Carlos Torres-Verdín & Shuang Gao - 2013 - Interpretation: SEG 1 (2):T177-T185.
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  50.  1
    Introduction to Special Section: Characterization of the Subsurface Stress, Deformation, and Pore Pressure.Gang Luo, Wei Gan, Rui Zhang, Junhua Guo & Jincai Zhang - 2020 - Interpretation 8 (2):SGi-SGii.
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