琼东南盆地深水重力流沉积旋回

通过3D地震资料,在琼东南盆地西部陆坡(15°30′00″~16°30′00″N)、早更新世至今的沉积地层中,自下而上依次识别了3套重力流沉积旋回,每套重力流沉积旋回由下部的块体搬运沉积体系和上部的水道-堤岸沉积体系构成.块体搬运沉积体系整体呈现为杂乱、半透明状的地震反射特征,底界面发育侵蚀沟谷,内部发育逆冲断层;水道-堤岸沉积体系整体表现为平行、连续同向轴的地震反射特征,局部半透明,发育弯曲水道、海鸥翼状堤岸、越岸沉积、决口扇和滑塌体.依据海底地形、重力流流动方向和中南半岛的山间河流分布推断越南中部山区是研究区的重力流物源,山间河流是主要的输送途径,指出陆架-陆坡的快速沉积物堆积是形成重力流沉积旋回的基本条件,探讨了海平面变化过程中的孔隙流体压力变化与重力流沉积体系类型之间的对应关系,并在理论上推测重力流旋回周期与更新世偏心率长周期(400~500 ka)的海平面变化一致.     

Magma flow inferred from magnetic fabrics in Wanning gabbro pluton and diabase dykes, Hainan

Measurements of anisotropy of magnetic susceptibility (AMS) were performed on a gabbro pluton and 7 diabase dykes in the Wanning area, southeast Hainan Island. Rock magnetism showed that pseudo-single domain (PSD) to multidomain (MD) Ti-poor magnetite carries the magnetic fabric in the gabbro pluton whereas MD Ti-poor magnetite carries the magnetic fabric in the diabase dykes. The corrected anisotropy degree (Pj ) in most specimens was found to be less than 1.2 which is indicative of a possible flow-related magnetic fabric. The AMS eigenvectors within each site are generally well grouped. The maximum susceptibility axes (K1 ) of the gabbro pluton are inclined towards the north at low angles (< 30°). K1 axes of the diabase dykes are inclined towards the NNW and SSE with dip angles of ≤ 30°. From this study, it appears that the emplacement mode of the gabbro pluton was characterized by intrusion from the north to the south at a low angle whereas the diabase dykes were emplaced from the NNW to the SSE at low to moderate angles. This was verified by comparison of the rock fabric to the magnetic fabric. All of this evidence leads to the conclusion that the Wanning gabbro pluton and diabase dykes were the products of pulsative intrusion from the same magma chamber in the area far to the north of Wanning, which suggests that basic rocks may exist beneath the Indosin- ian granite in the area to the north of Wanning.     

Thermal simulation experiment on the hydrocarbon regeneration of marine carbonate source rock

Hydrocarbon regeneration of marine carbonate source rock was simulated with thermal experiments in a laboratory. The results reveal that hydrocarbon regeneration does not simply continue the primary hydrocarbon generation process, and that, for marine carbonate source rock, discontinuous hydrocarbon generation differs greatly from the continuous generation. Several different features of hydrocarbon regeneration were observed in the experiments. First, the liquid hydrocarbon generation peak was always observed no matter what the initial maturity of the sample was. Moreover, the maturity and the liquid hydrocarbon yield corresponding to the peak varied with the sample’s initial maturity. Second, the hydrocarbon regeneration started earlier than the continuous one. In the experiments, the hydrocarbon could be re-generated when the sample maturity did not rise to any great extent. Third, the accumulative hydrocarbon-generating quantity during discontinuous generation was always more than that during continuous generation. And the hydrocarbon-generating quantity varied with the discontinuous generation history. Chemical kinetic analysis suggests that discontinuous hydrocarbon generation should not only be explained by the parallel reaction mechanism but also by the consecutive reaction mechanism which has been ignored in the traditional chemical kinetic model for continuous hydrocarbon generation.     

FMBEM求解直圆柱线性波绕射问题

运用快速多极子边界元法(Fast Multipole Boundary Element Method,FMBEM)求得单圆柱在线性波浪中的绕射问题的数值解.所谓的快速多极子边界元法就是采用快速多极子法(Fast Multipole Method,FMM)加速传统边界元法的求解速度.在文中通过求解二维的Helmholtz方程证明FMBEM法具有高精度和高效率,适用于求解大规模的数值问题.另外,给出了单圆柱线性平面波绕射问题中相关水动力学系数的数值计算结果.     

高能中子诱发半导体器件产生单粒子翻转的模拟计算

随着半导体及电子工艺技术的迅速发展,器件向着小尺度、低电压、低电荷、高集成度迈进,大气中子对航空及地面的电子系统造成的单粒子效应越来越显著.本文采用PHITS2.24蒙特卡罗程序及其事件发生器功能,借助于核反应模型与截面数据,验算了描述器件发生单粒子翻转能力的MBGR参数,并采用大气高能中子能谱,对SRAM器件的单粒子翻转率进行了计算与分析.这为我们今后模拟大气中子产生的各类单粒子效应提供了基本方法,也为将来开展相应的辐照实验提供了理论基础.     

基于病例-对照设计的中国马流感发生的集聚度探测研究

基于病例-对照设计、地理风险格局和集聚度探测等方法,开展我国马流行性感冒病例分布特点研究.研究显示,我国是马属动物的养殖大国,马流行性感冒在我国局部地区的马属动物群体中曾在较大范围发生.回顾性分析表明,我国马流感病例主要分布在西北和东北局部地区,2000～2007年病例集聚度探测表明,新疆伊犁州和巴音郭楞蒙古自治州交界地区坐标为(6460039.00,4277548.50)(P<0.001,R=7487976.06M,RR=273.94)病例区集聚度为最高,RR值达到273.94,显示该病例区及附近区域很有可能存在马流感疫情发生所需要的必要风险因素,提示应该加强对该区域马属动物的风险监管和主动监测.此外,在青海和甘肃等省、市和自治区的病例报道预示有沿新-青-甘-蒙一线传播态势.基于病例-对照设计和集聚度探测,初步明确了现阶段我国马流感发生风险主要集中在西北局部地区,应适时加强对我国新、甘、蒙等西北地区马流感的主动监测和马属动物的移动监管.