Cloning and mRNA expression of macrophage migration inhibitory factor (MIF) gene of large yellow croaker (Pseudosciaena crocea)   总被引：1，自引：0，他引：1  

MAO Yong  XU Bing  SU Yongquan  ZHANG Zhiwen  DING Shaoxiong  WANG Ding  WANG Jun 《海洋学报(英文版)》2010,29(3):63-73

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黑色页岩的 Re－Os 同位素定年   总被引：4，自引：0，他引：4  

杨競红  蒋少涌  凌洪飞  陈永权  冯洪真 《地球学报》2005,26(Z1):180-181

Re－Os 同位素是近年来发展起来的一种新的同位素技术，既可用于定年又能用于示踪。国际上如何对沉积岩进行精确定年一直是个难题。近年来的研究表示，Re－Os 同位素可以用于黑色页岩的精确定年，同时可用于示踪古海洋环境。笔者对华南下寒武统牛蹄塘组黑色页岩开展了 Re－Os 同位素定年研究，获得的等时线年龄为537±10Ma。  相似文献   

宽频带地震计的安装   总被引：1，自引：1，他引：0  

谢剑波  何寿清  吕金水  吴永权  张政平  黎珠博  王国望 《地震地磁观测与研究》2007,28(1):57-63

简要介绍了地震噪声的一些特点、环境因素影响宽频带地震计产生噪声的机制,并针对这些特点介绍了安装宽频带地震计的一些隔热保护方法和需要注意的事项,最后从检验系统安装与运行状况的角度,介绍了地震计的标定和台站噪声检测问题,列举了作者在宽频带测震台站建设中的工作实例.  相似文献   

Demand projection of natural gas in China based on the hybrid model of sector consumption     

GUO Xiaoqian  LIU Yongquan 《中国地质调查》2014,7(4):118-124

As a main clean energy in China, natural gas has received great attention under the requirement of the low-carbon development strategy. The demand projection of natural gas in China is very important for energy policymakers in future energy sources planning. The natural gas demand is influenced by a series of factors, which have a huge causal impact on demand projection. Therefore, the authors analyzed the influencing factors and the sector consumption of natural gas, and focused on the industrial, residential and transport sector to build a hybrid model. Based on the unit root tests, co-integration test and Granger causality test, the influencing factors of the natural gas demand were identified. Then the grey model and regression analysis were utilized to predict the demand for each factor. Finally, based on the projection above, the total natural gas demand for China will be 6 378.6×10⁸ m³ in 2025.  相似文献   

镜质体反射率热演化规律研究          下载免费PDF全文

阙永泉  郑伦举  秦建中  邱楠生 《地质科学》2014,(3):842-849

镜质体反射率的演化并不是人们传统意义上认为的随着温度（深度）的增加成指数增加,而是分阶段演化的。通过对有机质热模拟实验数据和自然演化数据进行分析后发现镜质体反射率的演化可以分为明显的3段：1）缓慢变化阶段,随着温度的增加镜质体反射率缓慢地变化,2）中等快速阶段,随着温度的增加镜质体反射率相比较前一阶段增加速率有明显的加大,3）快速增加阶段,随着温度的增加镜质体反射率呈指数快速增加。这种分阶段的演化是由镜质体本身的化学组成和化学结构所决定的。镜质体反射率演化阶段的划分对于热历史的恢复以及认识镜质体的热演化机制和规律具有重要的意义。  相似文献   

塔里木盆地寒武系—奥陶系烃源岩油源特征与超深层油气来源     

张科  苏劲  陈永权  马巳翃  张海祖  杨春龙  方玙 《地质学报》2023,97(6):2026-2041

塔里木盆地寒武系—奥陶系烃源岩的生源特征及其对超深层油气贡献是塔里木盆地超深层海相油气勘探面临的关键地质问题。根据分子与同位素地球化学分析和生烃热模拟实验研究,系统梳理油源对比的地球化学参数,认为原油中C26~C30甾烷的分布、伽马蜡烷指数、三环萜烷与五环萜烷比值和正构烷烃同位素等油源示踪指标,易受热演化程度、生物降解和水岩氧化还原作用影响,掩盖母源输入和沉积环境的差异。正构烷烃奇偶优势,异常的三环萜烷分布,全油和正构烷烃δ13C同位素明显偏重以及高含量的多环芳烃的出现主要归因于高过成熟热演化作用、低温热液或侵入岩浆等异常热事件的影响,而并非反映—O1烃源岩中生烃母质的地球化学特征。局部的硫酸盐热化学还原反应导致无机硫并入形成次生的噻吩类化合物,造成有机硫同位素值明显升高,无法反映母源特征,目前被选做寒武系典型烃源岩和端元油的生烃母源特征很可能是经历多种次生地球化学作用改造的结果。通过分析寒武系—奥陶系两套中等热成熟度烃源岩的形成环境和生物母质类型,表明塔里木盆地台盆区寒武系—奥陶系烃源岩的油源特征差异主要受控于沉积相,塔北中西部海相原油主要与透光厌氧环境烃源岩有关,塔中地区原油主要来源于深水盆地相烃源岩。重新建立不同物化性质原油与高过成熟烃源岩之间可靠的油 源对比参数,需要同时考虑成熟度和次生改造等复杂地球化学作用的多重影响才能确定其成因和来源。  相似文献   

日本囊对虾一种具有双结构域的新型C-型凝集素的分子特性和表达分析   总被引：1，自引：0，他引：1  

ZHANG Man  MAO Yong  WANG Jun  FENG Wenrong  SONG Xiaohong  SU Yongquan 《海洋学报(英文版)》2015,34(2):74-83

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碳酸盐岩构造裂缝发育模式探讨   总被引：2，自引：0，他引：2  

潘文庆  侯贵廷  齐英敏  张鹏  陈永权  鞠玮 《地学前缘》2013,20(5):188-195

从影响碳酸盐岩构造裂缝发育的主要因素入手,结合研究实例解剖分析,分别从岩性、层厚、风化作用、断裂作用、褶皱作用和区域构造应力场以及热液改造7个方面探讨了各种因素如何控制构造裂缝的发育程度和分布规律,并提出各种因素分别控制裂缝发育的概念模型。在考虑单一条件下,认为较粗粒的碳酸盐岩比较细的碳酸盐岩更易发育裂缝;薄层比厚层更易发育裂缝;风化壳顶部比下部更易发育裂缝;断裂附近比远离断裂更易发育裂缝;褶皱的转折端比翼部更易发育裂缝;区域应力场的应力集中部位更易比其他地区发育裂缝。热液改造裂缝可分为水力作用型和后充填型。  相似文献   

Types and Origin of Dolostones in Tarim Basin, Northwest China:Petrographic and Geochemical Evidence     

CHEN Yongquan  ZHOU Xinyuan  JIANG Shaoyong  ZHAO Kuidong 《《地质学报》英文版》2013,87(2):467-485

In the Tarim Basin of northwestern China hydrocarbon deposits have been discovered in parts of the thick strata of Cambrian dolostones. Based on petrographic study, six types of dolostone have been distinguished: Type-1, pink mud-bearing silty crystalline dolostone (PMSD); Type-2, gypsum- and salt-bearing fine crystalline dolostone (GSFD); Type-3, fine crystalline dolostone with dolomite crystals with cloudy core and clear rim (CCFD); Type-4, deep gray mud-bearing silty crystalline dolostone (GMSD); Type-5, euhedral coarse crystalline dolostone (ECD); and Type-6, xenotopic coarse crystalline dolostone (XCD). Applying petrographic and geochemical methods, the genesis of the dolostones is studied in this paper. Normally, Type-1 dolostone shows U- and Mo-depleted characteristics, reflecting a more oxidized formation environment; High δ18O and the purple color are consistent with formation of Sabkha dolostones on a supratidal flat. Types 2, 3, 4 dolostones show strata formation, similar REE patterns and 87Sr/86Sr ratios with contemporaneous limestones, suggesting a penecontemporaneous origin from seawater. Types 5 and 6 dolostones commonly occur as interbedded rocks, indicating secondary genesis after diagenesis. Type-6 dolostone has the highest order degree (OD) values (average 0.86), the lowest oxygen isotope values and positive Eu anomalies, which are consistent with previously reported hydrothermal dolostones. Differently, Type-5 shows euhedral texture, higher δ18O value, similar REE characteristic and 87Sr/86Sr ratios in comparison with contemporaneous limestones, suggesting that this type might have been dolomitized by down-transferring evaporated seawater during shallow burial stage. Dolostone fluid sources, formation environments and crystallizing dynamics are summarized and possible genetic models for the six types are proposed.  相似文献   

The construction of high precision geostrophic currents based on new gravity models of GOCE and satellite altimetry data     

Wenyan Sui  Junru Guo  Jun Song  Zhiliang Liu  Meng Wang  Xibin Li  Yanzhao Fu  Yongquan Li  Yu Cai  Linhui Wang  Lingli Li  Xiaofang Guo  Wenting Zuo 《海洋学报(英文版)》2021,40(3):142-152

The new gravity field models of gravity field and steady-state ocean circulation explorer(GOCE), TIM_R6 and DIR_R6, were released by the European Space Agency(ESA) in June 2019. The sixth generation of gravity models have the highest possible signal and lowest error levels compared with other GOCE-only gravity models, and the accuracy is significantly improved. This is an opportunity to build high precision geostrophic currents. The mean dynamic topography and geostrophic currents have been calculated by the 5 th(TIM_R5 and DIR_R5), 6 th(TIM_R6 and DIR_R6) release of GOCE gravity field models and ITSG-Grace2018 of GRACE gravity field model in this study. By comparison with the drifter results, the optimal filtering lengths of them have been obtained(for DIR_R5, DIR_R6, TIM_R5 and TIM_R6 models are 1° and for ITSG-Grace2018 model is 1.1°). The filtered results show that the geostrophic currents obtained by the GOCE gravity field models can better reflect detailed characteristics of ocean currents. The total geostrophic speed based on the TIM_R6 model is similar to the result of the DIR_R6 model with standard deviation(STD) of 0.320 m/s and 0.321 m/s, respectively. The STD of the total velocities are 0.333 m/s and 0.325 m/s for DIR_R5 and TIM_R5. When compared with ITSG-Grace2018 results, the STD(0.344 m/s) of total geostrophic speeds is larger than GOCE results, and the accuracy of geostrophic currents obtained by ITSG-Grace2018 is lower. And the absolute errors are mainly distributed in the areas with faster speeds, such as the Antarctic circumpolar circulation, equatorial region, Kuroshio and Gulf Stream areas. After the remove-restore technique was applied to TIM_R6 MDT, the STD of total geostrophic speeds dropped to 0.162 m/s.  相似文献