墨西哥湾盆地新生代沉积特征分析

通过收集、整理国内外学者的研究成果,总结了墨西哥湾盆地新生代的沉积特征及其与油气成藏的关系。分析认为,由于受古新世和早始新世的拉腊米构造运动的影响,墨西哥湾盆地新生代沉积时大量陆源碎屑不断进入盆地,使其海岸线、陆架和陆架边缘在新生代期间不断向盆地方向迁移,最终在陆棚处沉积巨厚的河流—三角洲沉积物;沉积中心的迁移控制了该区油气田的分布,而三角洲相控制了新生界油气富集,另外深水河道砂体、浊积扇砂体等是油气富集的重要相带。     

南黄海北部表层沉积物中生物标志物的组成特征及其地球化学意义

通过对南黄海北部14个站位的19个表层沉积物样品进行了粒度、有机碳、GC-FID和GC-MS-MS测定,探讨沉积物有机质中生物标志物组成特征及地球化学意义。研究区表明,沉积物有机碳含量较高,正构烷烃呈双峰分布,具有明显奇偶优势、平均L/H为0.36,说明沉积物中陆源高等植物贡献占优,分析对比表明其沉积物可能主要来自古黄河输入。类异戊二烯烃Pr/Ph均值0.46,表明有机质沉积于强还原环境;Pr/C₁₇和Ph/C₁₈值均小于1,并且随深度有减小的趋势,反映了研究区微生物的降解作用。甾类化合物C₂₉豆甾烷>C_（?）胆甾烷>C₂₈麦角甾烷,说明萜类化合物和甾类化合物主要为陆相输入。较高OEP值、高丰度的藿烯和莫烷及甾烷S构型含量均反映了现代沉积物中有机质未熟-低熟特征,但由于原始母质影响和微生物发育,Ts/Tm和C₃₁αβS/（S+R）、C₃₂αβS/（S+R）、C₃₃αβS/（S+R）和C₂₉αββ/（ααα+αββ）值较高。     

南黄海盆地中部隆起海相上构造层分布及断裂系统特征

南黄海盆地中部隆起区发育2套海相构造层,以下志留统高家边组泥岩滑脱带为界可划分为海相上构造层和海相下构造层。海相上构造层构造相对较复杂,以冲断结构为主,褶皱及叠瓦状逆冲断裂发育。对南黄海盆地中部隆起区多道地震资料进行处理解释表明,中部隆起区广泛发育海相上构造层,平面上总体表现为自西向东厚度呈厚—薄—厚的沉积格局。断裂系统发育,以近EW向断裂最为发育,其次为NE向断裂,NW向断裂则较为零星。构造应力以挤压和走滑为主,主要发育挤压、压扭和张扭3种构造样式。     

IMPACT OF THE HEATINC OVER SOUTH ASIA UPON THE SUBTROPICAL HIGH OVER WEST-PACIFIC

A case is reported, during which the Subtropical High over the Western Pacific(hereafter, SHWP in abbreviation)shifted northwestward and met-yu at Chaniiang River valley ended. Several numerical experiments on SHWP activity influenced by the heating over south Asia monsoon area are carried out, and the statistic significance of the results is checked. The results indicate that the enhancement of positive heating over South Asia will motivate a wave-like series of anomaly centers, which propagate northeastward from the maximum heating center.so that a strong positive potential height anomaly center will set up from North China to Japan at Day 3 result in the enhancement of SHWP. Comparison of the influence upon SHWP by the heating over south Asia monsoonarea with that over ITCZ area south to SHWP is also carried out. It is pointed out that the heating over South Asiamonsoon area tends to favor SHWP northward movement while the heating over ITCZ area tends to thvor SHWP westward stretching. As for the time to begin to influence on SHWP, the heating over south Asia monsoon areafavors the enhancement of SHWP atter Day 3 while that over ITCZ south to SHWP effects after Day 5.     

基于统计与动力相结合的南极夏季海冰跨季节预测

选取美国国家环境预测中心气候预测系统(CFS)第二版预测的南大洋(40^oS—80^oS)夏季海温、海洋性大陆地区(100^oE—130^oE,10^oN—15^oS)春季海温以及南半球热带外(20^oS—90^oS)春季海平面气压3个预测因子,利用奇异值分析的方法提取相关信息,采用回归模型对南极夏季海冰场进行预测。从该模式对1983—2018年南极夏季海冰密集度异常值的回报效果看,模型的预测技巧较CFS原始预测有显著的提高。对单格点上预测与实测的时间相关系数提高到0.76;从交叉检验的结果来看,预测技巧较CFS同样有显著提高;从对南极海冰范围的预测来看,该模型的预测效果最好,明显优于CFS原始预测和持续性预测。这些结果表明,该模型具有较高的预测性能。