黔中三叠纪地层研究新进展

通过对黔中地区区域地质调查，在二叠系—三叠系过渡层中发现了一系列的韵律层，并通过岩性岩相、矿物学、地球化学和地层古生物学研究，认为过渡层中韵律层是远源火山碎屑重力流沉积产物，并据古生物、沉积学、地层学研究将过渡层归属于三叠系。原安顺组下部“大汪段”之上、下发现大量牙形刺化石，根据岩性及古生物特征，将“大汪段”归入大冶组。黔中—黔南中三叠统陆源碎屑体系的物源来自江南古陆；菊石、双壳类化石层是浊流作用形成的事件沉积层。     

深水开发的新型立管系统——钢悬链线立管(SCR)

1种全新的深水立管系统——钢悬链线立管（Steel Catenary Riser,SCR）在翠西哥湾（Golf of Mexico）、坎普斯湾（Campos Basin）、北海（North Sea）和西非（West Africa）得到了成功应用。它的适用水深为300～3000m,且适用现有任何浮式结构,从浅水的固定式平台到极深水的浮式生产储运系统（FPSO）。因此,它取代了传统的柔性立管和顶张力立管,成为深水油气开发的首选立管,被认为是深水立管系统的成本有效的解决方案。     

深水钻井中浅水流灾害问题及其地球物理识别技术

在深水钻井中,浅水流是一种常见的地质灾害。中国正在进行深水油气勘探,十分有必要开展这方面的地质灾害研究。介绍了浅水流的形成机制及地球物理特性。目前用于识别和预测浅水流的手段有测井和反射地震两大类方法。主要介绍了几种用于参数提取的地震反演方法,如传统Dix反演、叠后振幅反演、层析反演、叠前振幅反演等。     

国外深水钢悬链线立管研究发展现状

介绍国外在新型深水立管系统--钢悬链线立管关键技术方面的研究发展现状,论述浮体一、二阶运动对钢悬链线立管疲劳寿命的影响、浮体升沉运动对钢悬链线立管触地点疲劳寿命的影响;钢悬链线立管与海底相互作用机制的实验研究及结果;钢悬链线立管涡致振动与疲劳的研究现状.并简要论述钢悬链线立管触地点问题的研究结论.     

中国南海北部珠江口-琼东南盆地钻井岩屑地球化学特征及深水区天然气聚集特征

The Qiongdongnan Basin and Zhujiang River(Pearl River) Mouth Basin, important petroliferous basins in the northern South China Sea, contain abundant oil and gas resource. In this study, on basis of discussing impact of oil-base mud on TOC content and Rock-Eval parameters of cutting shale samples, the authors did comprehensive analysis of source rock quality, thermal evolution and control effect of source rock in gas accumulation of the Qiongdongnan and the Zhujiang River Mouth Basins. The contrast analysis of TOC contents and Rock-Eval parameters before and after extraction for cutting shale samples indicates that except for a weaker impact on Rock-Eval parameter S_2, oil-base mud has certain impact on Rock-Eval S_1, Tmax and TOC contents. When concerning oil-base mud influence on source rock geochemistry parameters, the shales in the Yacheng/Enping,Lingshui/Zhuhai and Sanya/Zhuhai Formations have mainly Type Ⅱ and Ⅲ organic matter with better gas potential and oil potential. The thermal evolution analysis suggests that the depth interval of the oil window is between 3 000 m and 5 000 m. Source rocks in the deepwater area have generated abundant gas mainly due to the late stage of the oil window and the high-supper mature stage. Gas reservoir formation condition analysis made clear that the source rock is the primary factor and fault is a necessary condition for gas accumulation. Spatial coupling of source, fault and reservoir is essential for gas accumulation and the inside of hydrocarbon-generating sag is future potential gas exploration area.     

深海环境中溢油输移扩散的初步数值模拟

通过对溢油在深海环境中的输移过程及行为特点的分析,初步建立基于拉格朗日积分法的深海溢油模型.该模型除了能够模拟油气混合物在真实深海环境中的共同输移与分离输移扩散过程,还考虑了石油溶解、气体溶解、天然气水合物形成与分解等行为变化对溢油运动轨迹的影响.应用该模型初步数值模拟了一次实际深海溢油试验,结果表明溢油在水下的空间分...     

厦门港疏浚弃土吹填造陆物理模型试验研究

通过厦门港潮汐水流整体物理模型试验，掌握了厦门港十万吨级深水航道二期工程疏浚弃土吹填造陆各方案实施前后港池航道水流流态，为规划设计单位和决策部门利用疏浚弃土吹填造陆提供可靠的科学依据，试验结果表明，海沧吹填工程可作为一期吹填方案，鸡屿西吹填造陆工程可作为海沧吹填工程的后续工程，仅从水流角度考虑，象鼻嘴吹填造陆方案1是可行的。     

Tripod measured residual currents and sediment flux: Impacts on the silting of the Deepwater Navigation Channel in the Changjiang Estuary

Four bottom-mounted instrument-equipped tripods were deployed at two sections spanning the region characterized by severe sedimentation rates in the Deepwater Navigation Channel (DNC) along the North Passage of Changjiang Estuary in order to observe currents, near-bed suspended sediment, and salinity. Seaward residual currents predominated in the up-estuary section. In contrast, a classical two-layered estuarine circulation pattern occurred in the down-estuary section. Flow moved seaward in the upper layer and a heavier inflow, driven by the salinity gradient, moved landward in the lower layer. The near-bed residual currents in the up-estuary section and the down-estuary section acted in opposing directions, which implies that the region is a convergence zone of near-bed residual currents that trap sediment at the bottom. The maximum salinity gradient at the maximum flood current indicates the presence of a strong front that induces sediment trapping and associated near-bottom convergence of sediment, which explains the high sedimentation rates in this section of the estuary.