滨北 meaning in Chinese
hamakita
Examples
- Application of easy ro model to the research of thermal evolution in binbei
法在滨北地区热演化史中的应用 - Besides one or two samples showing type i , the organic matters of source rocks in binbei region are mostly type a , and some are b or
滨北中浅层源岩有机质以a型为主，其次为b型，再次为型，只有个别样品显示型特征。 - In this paper , a quantitative chemical dynamic model is presented which calculates the ratio of organic matters generating oil and gas with binbei region ' s thermal history on each stage , area , layer source rocks
结果表明，滨北中浅层源岩的总生油量为163亿吨、排油118亿吨，生气28500亿m ~ 3 、排气16800亿m ~ 3 。 - Toc in the source rocks of the third section and the fourth section of nenjiang , mingshui group , sifangtai group , cenozoic is lower . the average of toc is 0 . 8 % ~ 0 . 9 % , and the samples of toc > 1 % are less 40 %
滨北地区嫩江组三、四段，明水组，四方台组和新生代地层中的泥岩有机碳普遍较低，均值仅为0 . 8 0 . 9 ， toc 1的样品均不足总样品的40 。 - According to the characteristic of sedimentary stratum and the study of geochemistry in binbei area , source rocks of each layer become thicker from north to south . source rocks of south depressed center heiyupao , south wuyuer sunkeness and other area on the binzhou railway are best development
根据滨北地区地层的沉积特点和地球化学研究，各层源岩表现为从北向南逐渐增厚，其中黑鱼泡凹陷中部以南、乌裕儿凹陷南部、临近滨州线的其它地区源岩发育最好。