中国近海皱纹盘鲍不同地理群体的遗传结构与变异研究

皱纹盘鲍(Haliotis discus hannai Ino)是我国重要的经济海洋生物资源，以其营养价值高、味道鲜美而居海产八珍之首。由于资源的过度采捕、日益增加的养殖活动及海区环境污染等，可能会使皱纹盘鲍的遗传结构发生改变，继而影响到其适合度。为了种质资源的保护和可持续利用，同时也为了进一步完善皱纹盘鲍苗种繁育技术工艺，对我国近海皱纹盘鲍野生群体的遗传结构和变异研究是很有必要的。 等位基因酶电泳技术是研究海洋贝类遗传结构与变异的重要手段之一。目前世界上已有近百种海洋贝类的遗传结构和变异得到研究(张国范，1992；张国范等， 1993)，皱纹盘鲍日本分布区不同群体遗传结构和变异研究也有相关报道(Fu jino et al., 1978)。本文作者采用等位基因酶电泳技术，随机选取了24个等位基因位点，对皱纹盘鲍我国分布区内四个野生群体的遗传结构和变异进行研究，为我国皱纹盘鲍种质资源研究和可持续利用提供基础数据。     

Pressure evolution and hydrocarbon migration in the Baiyun sag, Pearl River Mouth basin, China

The Pearl River Mouth basin is one of the most important offshore basins in China. Petroleum exploration in the deep-water area is to start in the Baiyun sag in the basin. Due to the high cost of exploration in deep-water areas, the hydrocarbon migration and pressure evolution needs to be thoroughly probed before any actual exploration is to be done. Drilling results have indicated that the pore pressure is hydrostatic in shallow-water area. The mud diapirs found in the Baiyun sag indicate that there may be overpressure in the deep-water area. At present, little is known about hydrocarbon migration and pressure distribution in deep-water areas. On the basis of geological data from wells and basin modeling, the research comes to the following conclusions. (1) At least three episodic accumulations and releases of pressure had happened in the Cenozoic, which were closely related to the three regional tectonic movements: the Zhu-Qiong movement in the Late Eocene, the Nanhai movement in the Middle Oligocene and the Dongsha movement between the latest Middle Miocene and Late Miocene. The pressure release and associated hydrocarbon migration occurred primarily during the Dongsha movement, when most of the overpressure was released to hydrostatic pressure except for some overpressure in the deep-water area. (2) Both the measured pressure and the modeling results indicate that the pore pressure is hydrostatic pressure in the shallow-water area. Abnormally high pressure in the deep-water area is noted to be present. The difference of pressure distribution is caused by the lithologies, facies and faults. (3) The diapirs in the deep water cannot be driven by the overpressure because the maximum pressure is less than 9.0 MPa in the course of pressure evolution. (4) The fluids migrated to the shallow-water area and deep-water area along faults. Some faults connected the deep-water fans with the hydrocarbon source. Huge oil and gas fields may be formed in the deep-water area more favourably than in the shallow-water area. Translated from Earth Science-Journal of China University of Geosciences, 2006, 31(2): 229–236 [译自: 地球科学—中国地质大学学报]     

Application of zoom FFT technique to detecting EM signal of SLF/ELF

Introduction EM technique of artificial SLF/ELF (Super low frequency/extremely low frequency, their frequency ranges from 0.1 to 300 Hz) can be used to investigate crustal conductivity structure. The SLF/ELF artificial signal is very stable and transmitte…     

不同成因原油全扫描定量荧光特征及其影响因素

为揭示不同成因类型原油的三维全扫描荧光特征及其主控因素,对50个不同成因类型的原油的三维荧光特征进行了分析。原油样品代表了未熟—低熟至高成熟度范畴原油、淡水与咸水湖相、沼泽相成因原油、高蜡低硫与低蜡高硫油、常规油与重质油等类型。结果表明,分析原油三维荧光谱图及其定量参数有所差异。原油的荧光强度随芳烃含量增加而增加,沼泽相高蜡油荧光强度总体高于湖相原油;荧光强度随成熟度增加而降低、荧光主峰波长随成熟度增加而变短,反映芳烃总量与相对高分子量芳烃丰度具有降低趋势。稠油的荧光谱图不同于常规油,具有波长分布范围宽、主峰不明显等特征。成熟度、母源岩有机质类型与生源、次生改造等多种因素对原油的三维荧光特征有控制作用。     

矿井地质工作方法浅析 --以开滦荆各庄矿为例

通过 对 荆各 庄矿 构 造条 件的 基 本规 律的 分 析,查 找 造成 工作 失 误的 原因 ,阐 述 对井 田 地 质条 件 的 再 认识 ,揭示总 结交 流 矿井 地质 工 作的 基本 方 法。     

国际性区域经济合作进展效果评价

随着世界范围内区域集团化实践的扩展和深入,对区域集团化进展效果的评价成为国际学术界关注的热点问题。为了加强对国内开展地区经济技术合作的理论指导和实践总结,对有重要借鉴参考意义的有关研究成果进行初略概括和总结,主要从区域发展总体效果、区域集团化的贸易效应、投资效应与国际产业和技术转移的区域效果四个方面对主要研究结论和争议观点进行归纳分析。     

鼻咽癌放射治疗前后的CT表现对比分析

鼻咽癌是常见恶性肿瘤之一。为了提高对鼻咽癌放射治疗前后ＣＴ表现的认识与诊断,本文回顾性对比分析了有完整病史资料及病理结果,并经ＣＴ检查的鼻咽癌者８８例的放射治疗前后的ＣＴ表现,继而评价放射治疗对鼻咽癌的治疗效果,从而确定是临床治愈,好转或复发,给临床下一步治理提供可靠的依据。     

第三环境工程地质问题与内昆铁路岔河至威宁段的线路选择

首次讨论了第三环境工程地质问题,举出了在大型环境工程地质勘查中应用第三环境工程地质问题这一观点的成功实例。指出在进行第三环境工程地质问题的勘查与研究人员必须具有更加丰富的经验和广泛的知识,方能取得良好效果。     

辽宁二道沟金矿床矿物地球化学特征

对二道沟金矿床矿物学的详细研究和对比表明,该矿床中低温热液矿物组合和低温热液蚀变十分发育,与典型的冰长石－绢云母型浅成热液金矿的矿物组合十分相似,属于与流纹熔冉及其火山碎屑岩密切相关的浅成热液型金矿床。     

辽宁二道沟金矿床稳定同位素地球化学研究

对石曲中流体包裹体的氢氧同位素研究表明,二道沟金矿床含矿热水溶液的δＤ为－７１‰－－１０２．５‰,δ＾１８ＯＨ２Ｏ为１．３５‰－６．７‰,它们落入２００与３００℃时大气降水与火山岩发生水岩交换的演化线所夹的区域内,表明热水溶液主要来自源于大气降水的地下水,而不直接来源于岩浆热液。