ODP204航次天然气水合物的可能有利储层——浊积层   总被引：3，自引：1，他引：3  

龚建明  张莉  陈建文  Young-Joo LEE  王红霞  闫桂京 《现代地质》2005,19(1):21-25

为了解岩性在天然气水合物分布中的作用, 利用岩矿鉴定、扫描电镜和能谱法对ODP204航次的 4个站位 10个钻孔共计 115个沉积物样品进行分析, 发现沉积物中矿物成分基本相近, 以粘土矿物为主, 含少量以石英为主的陆源碎屑。样品中含有丰富的硅藻和有孔虫等微体化石, 可形成硅藻粘土—硅藻土、有孔虫硅藻土或凝灰质硅质生物粘土。石英碎屑大多呈棱角状, 粒径小、含量少, 同时, 样品中可见透镜体、团块或旋涡状层状结构以及杂乱堆积的斑杂构造。上述特征表明沉积物为含有大量深海或半深海的浊流沉积物或其夹层。由于钻井岩心中有相当部分的天然气水合物样品分布在上述沉积物中, 推断这些浊流沉积物很可能是ODP204航次天然气水合物的有利储层。  相似文献   

生态工法评估指标的建立   总被引：1，自引：0，他引：1       下载免费PDF全文

李锦育 《水科学进展》2005,16(3):361-367

基于集水区的尺度下,利用几种相关指标,以生物性与非生物性作一区隔,并进一步与生态工法施工准则加以结合,建立了一评估的方法论,探讨了工法施工之成效性。建立长期的河川水质监测计划,以了解在施工前、中及施工后的水质变动情形,避免工程对河川生态环境造成破坏。生态工法在指标的选择上应包含不同尺度的考量,以河川流域管理之完整性为主,藉由多样化的评估指标,提供决策者在拟定计划时能参考运用;另一方面也需运用生物指标的监测,提供具生态考量之工程规划参数,使工程施工能兼顾生态环境。  相似文献   

Application of Dangerous Probability Function in Risk Estimation of Surface Rupture Earthquake：Taking the Lingwu Fault in Ningxi1 Region as on Example     

Chai Chizhang  Zhang Wenxiao  Liao Yuhu  Xu Wenjun  Shen Xuhui  Tian Qinjian  Wei Kaibo  Chen Zhengwei 《中国地震研究》2002,16(1):60-70

Based on the fitting on paleoearthquake data of intra-plate regions in the northern part of Chi-na and giving a statistical model of time interdependence,the potential damage earthquakes in a definite future period and characteristics of present shocks along the Lingwu fault have been analyzed by using dangerous probability function and some new data concerned.We have in-ferred that the fault has entered a period that earthquakes will probably occur.There exists a potential danger that a strong earthquake with Ms7.0-7.5 will occur in 10-100a.  相似文献   

Contrast in Fluid M etallogeny between the Tianmashan Au-S Deposit and the Datuanshan Cu Deposit in Tongling, Anhui Province     

LEE Hyun Koo 《《地质学报》英文版》2003,77(1):116-124

A comprehensive contrast of ore-forming geological background and ore-forming fluid features, especially fluid ore-forming processes, has been performed between the Tianmashan and the Datuanshan ore deposits in Tongling, Anhui Province. The major reasons for the formation of the stratabound skarn Au-S ore deposit in Tianmashan and the stratabound skarn Cu ore deposit in Datuanshan are analyzed in accordance with this contrast. The magmatic pluton in Tianmashan is rich in Au and poor in Cu, but that in Datuanshan is rich in Cu and Au. The wallrock strata in Tianmashan contain Au-bearing pyrite layers with some organic substance but those in Datuanshan contain no such layers. Moreover, the ore-forming fluids in Tianmashan are dominantly magmatic ones at the oxide and sulfide stages, but those with high content of Cu in Datuanshan are mainly groundwater fluids. In addition, differences in compositional evolution and physicochemical condition variation of the ore-forming fluids result in gradual dispersion  相似文献   

NUMERICAL SIMULATIONS OF SCOUR AND DEPOSITION IN A CHANNEL NETWORK     

Hong-Yuan LEE  Hui-Ming HSIEH 《国际泥沙研究》2003,18(1)

1 INTRODUCTION Evolution of the river bed in alluvial channels has been studied by many researchers using analytical and numerical approaches. The use of analytical approach alone is insufficient for solving natural river engineering problems. With rapid growth in computer technology, numerical models have become a popular means for the study of mobile bed hydraulics. During the past decade, several numerical models have been developed. Most of the computer codes, such as HEC2SR (Si…  相似文献   

渭河断裂西段活动差异性分析   总被引：17，自引：0，他引：17  

冯希杰田勤俭  申旭辉 《地质论评》2003,49(3):233-238

渭河断裂是一条纵贯渭河盆地中部的大断裂，对渭河盆地的形成和发展乃至盆地内的地震活动都具有控制作用。本文将宝鸡峡口以东，西安市草滩镇以西的渭河断裂西段作为研究区。从渭河断裂北侧黄土台源地貌存在的分级现象、自西向东渭河断裂新近系错距大小非均匀变化、渭河断裂西段断坎地貌差异等方面的分析，讨论了渭河断裂西段存在的活动差异性，认为以千河断裂、岐山-马召断裂和泾河推测断裂为分界点，渭河断裂西段可分为三个亚段，各个亚段在断裂活动时间、活动强度等方面均有明显的差异。通过对渭河断裂西段所处新构造环境的分析，认为第四纪以来渭河盆地西部地壳的向东掀斜拾升运动是造成渭河断裂西段出现差异性活动的根本原因。  相似文献   

Fetch and Footprint of Turbulent Fluxes over Vegetative Stands with Elevated Sources   总被引：1，自引：0，他引：1  

Xuhui Lee 《Boundary-Layer Meteorology》2003,107(3):561-579

In this study, Raupach's localized near-field (LNF)theory is combined with appropriate parameterizations ofthe turbulence inside a canopy to investigate how airstability and source configuration influence the fluxfootprint and flux adjustment with fetch in theroughness sublayer. The model equations are solvednumerically. The flux footprint from the LNF predictionis in general more contracted than the prediction basedon the inertial sublayer similarity functions. Invery unstable conditions, the near-field effect causes thefootprint of the elevated canopy source to locatefurther upwind than that of the ground-level source, andthe combined footprint can become negative in situationswhere the two sources are of opposite sign. The fluxfootprint and flux adjustment with fetch in theroughness sublayer are sensitive to source configurationand the parameters specifying wind speed and theLagrangian time scale inside the canopy.  相似文献   

对流边界层中泡状结构的大涡模拟研究   总被引：7，自引：3，他引：7       下载免费PDF全文

蔡旭晖  陈家宜 《大气科学》1997,21(2):223-230

本文提出“连续垂直运动区”的概念，对边界层中的对流泡状运动进行了重新定义。由此将对流边界层划分为上升泡区、下沉泡区和环境气流区，并利用大涡模拟提供的对流边界层数值模拟结果研究这种泡状运动的结构。研究结果较好地解释了一些有关泡状运动结构方面的似乎相互矛盾的观测事实，并揭示了对流泡状运动的一些新的特征。  相似文献   

小江断裂带中段盆地的发育阶段及其与区域构造运动的关系   总被引：4，自引：1，他引：4       下载免费PDF全文

宋方敏  俞维贤 《地震地质》1997,19(3):20-217

小江断裂带中段新生代发育的系列盆地，根据其发育阶段可分为始新世—渐新世、上新世—早更新世、中更新世—晚更新世和晚更新世—全新世４个阶段，并根据发育持续性可分为继承性、阶段性、复活性、新生性４种类型。由大比例尺填图所获资料及前人成果，介绍了各阶段盆地的分布特征和成因机制，讨论了盆地发育与区域构造运动、断裂活动的关系  相似文献   

江苏省主要作物农田水分盈亏量的研究   总被引：5，自引：0，他引：5       下载免费PDF全文

汤志成  张旭晖 《应用气象学报》1997,8(4):503-508

利用江苏省1980～1992年土壤湿度资料，根据土壤水分平衡原理，运用运筹学中的优化技术，结合本省的自然条件和作物生长实际情况，提出有效降水量、下层水分补给量等计算方法，建立了旱地和稻田农田水分盈亏量的计算模式，以便应用实时降水和土壤湿度等资料，计算全省农田水分盈亏量，及时提供农业气象情报服务。  相似文献