南海北部陆缘黏土矿物组合特征与地质意义

采用沉积矿物分析方法对南海北部九口探井渐新世—中新世沉积物进行系统的黏土矿物分析.结果表明:南海北部沉积物黏土矿物组成随时间及空间呈现规律性变化,黏土矿物伊/蒙转化深度具有自北向南逐步变浅的规律,与地温梯度升高变化趋势基本一致,这种黏土矿物伊/蒙转化的变化规律反映了南海北部洋陆过渡地壳减薄,莫霍面抬升,热流值升高的趋势.通过黏土矿物组合演变特征与热流变化趋势的相关关系,可以预测区域性温度场变化规律,加深对南海北部洋陆过渡地壳厚度变化的认识.     

东海风暴潮数值预报模式参数的敏感性分析

设计两个模拟台风,以北上型台风路径对东海风暴潮数值预报模式进行敏感性分析。采用高桥水文站的风暴潮计算结果,分析了台风引起的最大增水及出现时间对台风中心经度、纬度、中心气压和最大风圈半径的敏感程度。结果表明,最大风暴增水的数值对台风中心纬度并不敏感,对台风中心气压、最大风圈半径有一定的敏感,但也并不显著,而对台风中心经度最为敏感。最大增水出现的时间则对台风中心气压、最大风圈半径并不敏感,对台风中心经度和纬度较为敏感,尤其是纬度最为显著。在设计的两种模拟台风中,最大增水出现的时间表现出对台风中心纬度以及台风移速更为敏感.     

Magnetic characteristics and its environmental implications of core YSJD-86GC sediments from the southern South China Sea

Sediments of core YSJD-86GC （referred to as 86GC） collected from the southern South China Sea were selected for environmental magnetic studies. Combined with the published chronological framework, sediment magnetic properties were revealed for the study area since the MIS3 stage. The rock magnetic results indicate that low-coercivity magnetite is the main magnetic mineral within the sediments. Also, a certain amounts of hematite are present. The King plot and Day plot, which reflect the magnetic particle size, show that fine-grained pseudo-sin- gle-domain phase magnetic particles dominate the magnetic minerals in the sediments. Comparison of magnetic parameters and geochemical indicators show that magnetic properties of core 86GC sediments reflect a terrigenous input. Simultaneously, magnetic characteristics of the stud- ied sediment are influenced by the quantity of terrigenous sediment input, oxidation-reduction conditions of the provenance area, and the transportation environment and distance. Sea level fluctuation caused by global climate change was the main factor for variation in concentration of magnetic minerals and magnetic particle size of thestudied core sediments. Thus, variation of sediment magnetic properties in the study area can be used as an indirect indicator of sea level fluctuation.     

Millennial climate changes since MIS 3 revealed by element records in deep-sea sediments from northern South China Sea

High resolution elemental MD05-2903 from the northern South records in core China Sea were obtained from XRF scanning and grain size and mineral component analyses. The K/Ti curve reveals climate changes since MIS 3 on a millennial scale, representing one of the best such records so far from deep-sea sediments of the South China Sea. When compared our K/Ti record with other climate records from high latitude ice cores and from East Asia stalagmites, variations in the K/Ti record show some typical saw-shaped features of rapid climate changes in the Northern Hemisphere. Grain size analysis reveals a close relationship between variations in K/Ti and in the fine end-member grain size. XRD analysis confirms that high K/Ti layers were dominated by K-rich weathering minerals, especially illite, while low K/Ti layers contain low illite but high abundance of Ti-rich heavy minerals. Therefore, the K/Ti record reflects changes in the input and deposition of fine weathering minerals and heavy minerals in the northern South China Sea region during stadials and interstadials. These elemental changes were largely con- trolled by variations in rainfall, erosion, and fluvial trans- portation induced by East Asia Monsoon.     

中国需全力推进鲁日韩“小TPP自贸区”建设吗——“黄海经济圈”建设应是我国区域发展战略中的第一战略吗

中国正在全面崛起,经济和科技实力大大增强,但是在知识产权能力上与日本依然存在一定差距。日本依靠反向工程、改进创新、原始创新,以及纵向和横向的累积性、协同性、重构性集成创新跨越"海量"知识产权积累的"高墙",掌握"高墙"后的高级技术系统,使其在大部分的尖端技术领域都取得了关键性突破,甚至赶超俄罗斯和美国。因此,我们应强化与日本之间的技术交流和经济合作,尤其要大力推进"鲁日韩一体化战略"。     

动态最优插值方法及其同化应用研究

根据常规最优插值算法,在引入时间关联的基础上,详细推导了动态最优插值法的具体同化表达形式,利用这些公式,可以处理常见的在海洋观测数据同化中存在的时间错位问题.在陆架海模式HAM-SOM基础上,以7月份的渤海海表温度为例,验证了同化公式的可行性,并得到了较好的同化结果.验证结果表明:该方案能够兼顾观测数据与背景数据双方的特性,同化后的结果更加接近实际情况.     

High-precision U-series dating of Holocene corals from South China Sea by thermal ionization mass spectrometry (TIMS)

Using the isotopic diluting and thermal ionization mass spectrometric (TIMS) technique, the U-series dating procedure was established on the basis of measurement of national standard GBW04412. With this highly precise technique the Holocene corals from the South China Sea were dated. Comparison between this method and α-spectrometry was made. The results show that a thriving period of corals in the South China Sea appeared at 6 800-5 800 a BP, during which the paleosea level was the higher than at present in the Holocene.     

密度成像技术在南海西部油田地质导向中的应用

水平井施工过程中已广泛应用随钻地质导向技术,在持续发展储层随钻测绘等新技术过程中,密度成像技术在随钻地质导向技术中的应用仍然较为普遍。针对南海西部Z油田井控程度低、构造变化大、储层横向变化快等问题,引入了密度成像工具和相应的地质导向技术。借助高分辨率密度成像成果拾取精确的地层倾角,在此基础上分析落实构造形态,判断轨迹所处的相对位置;配合地质录井确定的岩性情况,避免局部相变造成的出层;从而为实时决策提供判断依据并指导地质导向。实施过程中首次提出并使用了过井轴视倾角的概念,改进了常规利用成像数据计算地层倾角的方法并通过实际对比验证;该区块目前已完钻4口水平井,平均长度580 m,优质储层钻遇率80%。结论认为：在密度变化明显的构造+岩性油藏中使用该技术,能有效降低构造不确定性等地质风险,提高优质储层钻遇率。     

基于SONIC软件的鄂霍次克海浅表陆坡可燃冰勘探研究

运用自主研发设计的SONIC软件,控制深海勘探设备Echo水声探测系统,对位于西北太平洋边缘的鄂霍次克海海底可燃冰甲烷释放情况进行勘探研究。重点对萨哈林岛东面浅表陆坡进行了大规模的水声测扫,通过采集回声信号,应用SONIC软件处理和成像后,实现了海底甲烷气体渗漏点（GF）、冷泉和海床的可视化。在发现甲烷气体渗漏点后,运用SONIC的成像功能,分析冷泉中甲烷气体浓度及形态的变化,运用GPS系统进行实时跟踪与定位,利用重力取样器等采样工具,在多个海域成功采集到了可燃冰岩心样本,并及时进行了分析,得到了该地区可燃冰中的甲烷排放速率和甲烷排放量等数据。另外,通过梳理本次考察的经验,对规范我国可燃冰资源调查方法也会产生积极影响。     

渤西地区新生代断裂体系特征及形成演化

为明确渤西地区新生代断裂体系发育特征,利用最新的三维地震资料及钻井资料,通过地震切片、方差体切片、断层活动速率等技术方法,重点从断裂几何学特征、性质及样式、运动学特征、构造演化动力学背景等方面对渤西新生代断裂体系发育特征进行了精细刻画。结果表明:研究区断裂发育存在北东、北西和近东西向三个优势方向,早期(古近纪)以发育张性断裂为主,后期叠加走滑作用,使得断裂复杂化;渤西地区新生代断裂体系演化经历了古新世-早始新世末的初始伸展、始新世中晚期强烈伸展、晚始新-早渐新世弱拉张-弱张扭、中-晚渐新世张扭-走滑、上新世至今强走滑等五个阶段。渤西地区新生代多期次、多阶段、不同性质复杂断裂体系是受区域应力场、沙垒田古隆起、基底先存断裂等因素综合作用的结果。