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Evaluation of Latent Tuberculosis Infection Using the ESAT6-CFP10 Skin Test Among International Freshmen With Diverse Skin Tones at a University—Nanjing City,Jiangsu Province,China,September 2023

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China CDC weekly 2024年第35期6卷 896-900,I0001页

作者： Peng Lu Rong wang Jingjing Xu Jianming wang Fangfang Du guozhi wang Shiming Cheng Limei Zhu Department of Chronic Communicable Disease Jiangsu Provincial Center for Disease Control and PreventionNanjing CityJiangsu ProvinceChina Department of Epidemiology School of Public HealthNanjing Medical UniversityNanjing CityJiangsu ProvinceChina Nanjing City Center for Disease Control and Prevention Nanjing CityJiangsu ProvinceChina Chinese Antituberculosis Association BeijingChina National Institutes for Food and Drug Control BeijingChina

Introduction:Newer skin tests,including the ESAT6-CFP10(EC)skin test,were recommended for diagnosing Mycobacterium tuberculosis(***)***,no data exist assessing the diagnostic performance of the EC skin test among foreign students with different skin ***:A cohort study at Nanjing Medical University screened incoming foreign *** EC skin test was used to assess for *** infection,and results were read at 24,48,72,and 96-hours ***:Among 96 participants,*** infection rates at 24,48,72,and 96-hours post-injection were 3.13%,7.29%,13.54%,and 9.38%,*** infection rates were lower among individuals with darker skin tones,the difference was not statistically significant(P=0.186),and variations were consistent across different measurement *** analysis revealed 5.3%in the continuousincreasing group,86.5%in the low-stable group,and 5.2%in the elevated-decreasing ***,participants in the elevated-decreasing group had lighter skin tones,with trajectory patterns consistent across different skin ***:The EC skin test is safe,and redness diameter is a more reliable indicator than *** should be collected within 48 to 72 hours,with verification at 72 hours crucial if initial results are ***,skin color does not affect EC skin test outcomes.

关键词： CFP10 Skin Nanjing

Composition and Origin of Ferromanganese Crusts from Equatorial Western Pacific Seamounts

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Journal of Ocean University of China 2015年第2期14卷 217-227页

作者： wang guozhi JANSA Luba CHU Fengyou ZOU Can SUN Guosheng State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu University of Technology Department of Earth Sciences Dalhousie University Key Laboratory for Geosciences State Oceanic Administration Chengdu University of Technology College of Earth Sciences Jilin University

In the equatorial western Pacific, iron-manganese oxyhydroxide crusts(Fe-Mn crusts) and nodules form on basaltic seamounts and on the top of drowned carbonate platform guyots that have been swept free of pelagic sediments. To date, the Fe-Mn crusts have been considered to be almost exclusively of abiotic origin. However, it has recently been suggested that these crusts may be a result of biomineralization. Although the Fe-Mn crust textures in the equatorial western Pacific are similar to those constructed by bacteria and algae, and biomarkers also document the existence of bacteria and algae dispersed within the Fe-Mn crusts, the precipitation, accumulation and distribution of elements, such as Fe, Mn, Ni and Co in Fe-Mn crusts are not controlled by microbial activity. Bacteria and algae are only physically incorporated into the crusts when dead plankton settle on the ocean floor and are trapped on the crust surface. Geochemical evidence suggests a hydrogenous origin of Fe-Mn crusts in the equatorial western Pacific, thus verifying a process for Fe-Mn crusts that involves the precipitation of colloidal phases from seawater followed by extensive scavenging of dissolved trace metals into the mineral phase during crust formation.

关键词： ferromanganese crusts biomarker hydrocarbon REE trace element hydrogenous origin

Formation and evolution of Sinian oil and gas pools in typical structures, Sichuan Basin, China

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Petroleum Science 2012年第2期9卷 129-140页

作者： Yuan Haifeng Liang Jiaju Gong Deyu Xu Guosheng Liu Shugen wang guozhi State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu University of TechnologySichuan 610059China College of Energy Resources Chengdu University of TechnologySichuan 610059China

The only major breakthrough in the exploration of the Sinian of the Sichuan Basin has been the Weiyuan gas field. Taking the typical structures in the Sichuan Basin as examples, an apatite fission track simulation was applied to constrain the thermal evolutionary history of the source rocks in this study. Combined with trap formation and evolution, the formation, destruction, and accumulation history of the Sinian reservoirs were analyzed from a dynamic perspective. The Sinian reservoirs underwent several primary stages： the paleo-reservoir formation and destruction in the late Silurian, hydrocarbon recharge in the Permian-Triassic, the cracking of oil to gas and dissolved-gas in the late Triassic-Mid-Late Jurassic, and the exsolution and accumulation of dissolved-gas as a result of episodic uplift since the Late Cretaceous. The exsolution process of dissolved-gas is of great significance to the accumulation of natural gas. The formation of the Weiyuan gas field is also related to this process. The Sinian in the Sichuan Basin has a broad exploration prospect, and exploration targets focused on the Leshan-Longnüsi Paleo-uplift tectonic zone with weak influences on potential hydrocarbon reservoirs from the late tectonism and transformation.

关键词： Apatite fission track Sinian reservoirs Sichuan Basin

Multi-Stage Hydrocarbon Accumulation and Formation Pressure Evolution in Sinian Dengying FormationCambrian Longwangmiao Formation, Gaoshiti-Moxi Structure, Sichuan Basin

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Journal of Earth Science 2016年第5期27卷 835-845页

作者： Juan Wu Shugen Liu guozhi wang Yihua Zhao Wei Sun Jinming Song Yanhong Tian State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu University of Technology Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education China University of Geosciences Chuanzhong Division of Southwest Oil & Gasfield Company Petro China

Sichuan Basin is a typical superimposed basin, which experienced multi-phase tectonic movements, meanwhile Sinian–Cambrian underwent complex hydrocarbon accumulation processes, causing exploration difficulties in the past 60 years. Based on the microscopic evidence of fluid inclusions, combined with basin-modelling, this paper determines stages and time of hydrocarbon accumulation, reconstructs evolution of formation pressure and dynamic processes of hydrocarbon accumulation in Sinian Dengying Formation-Cambrian Longwangmiao Formation of Gaoshiti-Moxi structure. Three stages of inclusions are detected, including a stage of yellow-yellowgreen fluorescent oil inclusions, a stage of blue fluorescent oil-gas inclusions and a stage of non-fluorescent gas inclusions, reflecting the study area has experienced a series of complex hydrocarbon accumulation processes, such as formation of paleo-oil reservoirs, cracking of crude oil, formation of paleo-gas reservoirs and adjustment to present gas reservoirs, which occurred during 219–188, 192–146 and 168–0 Ma respectively. During the period of crude oil cracking, Dengying Formation-Longwangmiao Formation showed weak overpressure to overpressure characteristics, then after adjustment of paleo-gas reservoirs to present gas reservoirs, the pressure in Dengying Formation changed into overpressure but finally reduced to normal pressure system. However, due to excellent preservation conditions, the overpressure strength in Longwangmiao Formation only slightly decreased and was still kept to this day.

关键词： Sichuan Basin Gaoshiti-Moxi structure Sinian-Cambrian hydrocarbon accumulation,formation pressure fluid inclusion.

Hydrocarbon Accumulation Process in the Marine Strata in Jianghan Plain Area, Middle China

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Acta Geologica Sinica(English Edition) 2014年第3期88卷 878-893页

作者： XU Guosheng ZHANG Lijun GONG Deyu wang guozhi YUAN Haifeng LI Changhong HU Xiaofeng State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu University of Technology Research Institute of Petroleum Exploration and Development PetroChina Exploration and Development Research Institute of Jianghan Oilfield Branch of Sinopec

Marine strata in the Jianghan Plain area are widely distributed with a total depth of more than 8,000 m from the Upper Sinian to the Middle Triassic. Six reservoir caprock units, named Z-C2, C2-O, S, D--C, P and T1, can be identified with each epoch. The geology, stratigraphy, drilling, oil testing and other basic data as well as the measured inclusion and strontium isotope data in the study area are used in the analysis of the formation and evolution process of marine petroliferous reservoirs in the Jianghan Plain area. This study aims to provide a scientific basis for the further exploration of hydrocarbons in the Jianghan Plain and reduce the risks by analyzing the key factors for hydrocarbon accumulation in the marine strata. Our findings show that in the Lower Palaeozoic hydrocarbon reservoir, oil/gas migration and accumulation chiefly occurred in the early period of the Early Yanshanian, and the hydrocarbon reservoir was destroyed in the middle-late period of the Early Yanshanian. In the Lower Triassic-Carboniferous hydrocarbon reservoir, oil/gas migration and accumulation chiefly occurred in the Early Yanshanian, and the hydrocarbon reservoir suffered destruction from the Late Yanshanian to the Early Himalayanian. The preservation conditions of the marine strata in the Jianghan Plain area have been improved since the Late Himalayanian. However, because all source beds have missed the oil/gas generation fastigium and lost the capacity to generate secondary hydrocarbon, no reaccumulation of hydrocarbons can be detected in the study area＇s marine strata. No industrially exploitable oil/gas reservoir has been discovered in the marine strata of Jianghan Plain area since exploration began in 1958. This study confirms that petroliferous reservoirs in the marine strata have been completely destroyed, and that poor preservation conditions are the primary factor leading to unsuccessful hydrocarbon exploration. It is safely concluded that hydrocarbon exploration in the

关键词： marine strata reservoir caprock unithydrocarbon accumulation process reservoirevolution Jianghan Plain area Middle China

The coupling of fluid flow and uplift since Late Cretaceous in Zoige area, western Sichuan

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Science China Earth Sciences 2011年第7期54卷 1043-1052页

作者： DENG Bin LIU ShuGen LI JuChu wang guozhi LIU Shun LI ZhiWu LI XiangHui State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu 610059 China

The uplift indicated by five AFT (apatite fission track) samples is more than 3400 m by multi-episodic uplift since Late Cretaceous in Zoige area; especially the processes of fast uplift in Late Cretaceous and Neogene have important influences on the stress of paleo-fluid. Based on field geology, macroscopic features of fracture, and geochemistry of fluid inclusions, we decipher the paleo-fluid process of episodic migration. In early uplift stage, the temperature of inclusions increased with the constant salinity, whilst both of them proportionally decreased in the mid-late stage, indicating the different tendency of heat-fluid warming and freshwater contamination at different time. Of particular importance are the features of episodic fluid flow, such as ESR ages, and features of multi-episodic migration that correspond well with the process of multi-episodic uplift. Thus, concerning the rock stress-strain behavior responding to uplift, we further discuss the spatio-temporal coupling effect of episodic migration and decompression in multi-episodic uplift, thereby to better understand petroleum geology in the region.

关键词： multi-episodic uplift paleo-fluid decompression in the uplift episodic migration Zoige area

Synthesis and characterization of wormhole-like mesoporous Ce_(0.6)Zr_(0.35)Y_(0.05)O_2 solid solutions

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Chinese Science Bulletin 2007年第2期52卷 175-180页

作者： wang guozhi ZHANG Lei DENG JiGuang DAI HongXing HE Hong ZI XueHong Laboratory of Catalysis Chemistry and Nanoscience Department of Chemistry and Chemical Engineering College of Environmentaland Energy Engineering Beijing University of Technology Beijing 100022 China

Nanoparticles of Ce0.6Zr0.35Y0.05O2 (CZY) solid solution have been prepared by the CTAB (hexadecyl-trimethyl ammonium bromide), CTAB-EG (ethylene glycol) templating, and CTAB-EG-NaCl (in which the pores of the precursor synthesized by the CTAB-EG method is filled by a certain amount of NaCl) method, respectively. The physical properties of these materials were characterized by means of tech-niques such as X-ray diffraction (XRD), high resolution scanning electron microscopy (HRSEM), transmission electron microscopy (TEM), selected area electron diffraction (SAED), and N2 adsorp-tion-desorption measurements. The CZY samples synthesized by the above three methods display wormhole-like mesoporous morphology and cubic crystal structures. The materials are narrow in pore size distribution (averaged pore diameter = 5.3―7.1 nm), high in surface areas (95―119 m2/g), and large in pore volumes (0.16―0.18 cm3/g). It has been demonstrated that the introduction of NaCl is capable of retaining the pore structures of solid nanomaterials at high-temperature calcination.

关键词：固溶体同质晶体结构合成方法微粒铈稀土元素

Fluid migration paths in the marine strata of typical structures in the western Hubei-eastern Chongqing area,China

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Petroleum Science 2013年第1期10卷 1-18页

作者： Xu Guosheng Liang Jiaju Gong Deyu wang guozhi Yuan Haifeng Cao Junxing Zhang Chengfu State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation(Chengdu University of Technology) Research Institute of Petroleum Exploration and Development SINOPEC Zhongyuan Oilfield Company

The western Hubei-eastern Chongqing area is an important prospective zone for oil and gas exploration in the central Yangtze area. Three representative structures, the Xinchang structure, Longjuba gas-bearing structure and the Jiannan gas field, were selected to analyze biomarker parameters in marine strata and to examine various types of natural gas and hydrocarbon sources. Fluid inclusions; carbon, oxygen, and strontium isotopic characteristics; organic geochemical analysis and simulation of hydrocarbon generation and expulsion history of source rocks were used for tracing fluid migration paths in marine strata of the study area. The Carboniferous-Triassic reservoirs in three typical structures all experienced at least two stages of fluid accumulation. All marine strata above the early Permian were shown to have fluids originating in the Permian rocks, which differed from the late stage fluids. The fluids accumulated in the late Permian reservoirs of the Xinchang structure were Cambrian fluids, while those in the late Carboniferous reservoirs were sourced from a combination of Silurian and Cambrian fluids. A long-distance and large-scale cross-formational flow of fluids destroyed the preservation conditions of earlier accumulated hydrocarbons. A short-distance cross-formational accumulation of Silurian fluids was shown in the late Permian reservoirs of the Longjuba structure with favorable hydrocarbon preservation conditions. The fluid accumulation in the Carboniferous reservoirs of the Jiannan structure mainly originated from neighboring Silurian strata with a small amount from the Cambrian strata. As a result, the Jiannan structure was determined to have the best preservation conditions of the three. Comparative analysis of fluid migration paths in the three structures revealed that the zone with a weaker late tectonism and no superimposition and modification of the Upper and Lower Paleozoic fluids or the Upper Paleozoic zone with the fluid charging from the Low

关键词： Western Hubei-eastern Chongqing area marine strata geochemical tracer fluid migration path

Multi-Stage Basin Development and Hydrocarbon Accumulations： A Review of the Sichuan Basin at Eastern Margin of the Tibetan Plateau

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Journal of Earth Science 2018年第2期29卷 307-325页

作者： Shugen Liu Bin Deng Luba Jansa Zhiwu Li Wei Sun guozhi wang Zhili Luo Ziquan Yong State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu University of Technology Chengdu 610059 China Geological Survey of Canada-Atlantic Dartmouth N.S. Canada

Sichuan Basin is one of the uppermost petroliferous basins in China. It experienced three evolutionary phases which were marine carbonate platform （Ediacaran to Late Triassic）, Indosinian-Yanshanian orogeny foreland basin （Late Triassic to Late Cretaceous） and uplift and tectonic modification （Late Cretaceous to Quaternary）. The present-day tectonics of the Sichuan Ba- sin and its periphery are characterized by three basic elements which are topography, basement type and surface structure, and two settings （plate margin and interior）. Therefore, be subdivided into five units which have different structure and tectonic history. The basin contains five different sets of source rocks with thickness up to 2 500 m. These source rocks were well preserved due to the presence of Middel-Lower Triassic evaporites （〉-200 m） and thick terrestrial sediments filling in the Indosinian-Yanshanian foreland basin （〉3 000 m）. The uplift and erosion since Late Cretaceous has significant influence on cross-strata migration and accumulation of oil and gas. The multi-phase evolution of the basin and its superimposed tectonic elements, good petroleum geologic conditions and diverse petroleum systems reveal its bright exploration prospects.

关键词： multi-stage basin hydrocarbon accumulation Sichuan Basin eastern margin of the Tibetan Plateau.