铁法盆地含煤沉积旋回的构造控制作用     

王宇林  刘锦  魏恒飞  王铁晖  王刚 《煤田地质与勘探》2010,38(6):1

为探索铁法盆地含煤沉积旋回的成因,在应用沉积相分析方法揭示该盆地含煤沉积旋回特征的基础上,依据盆缘断裂活动引起可容空间的变化,进而控制沉积物体积分配、沉积相类型及其空间配置的原理,对其含煤沉积旋回的构造控制作用进行了深入研究。分析认为,在盆缘断裂活动导致可容空间减小和沉积充填速率较高的条件下,形成了盆缘断裂内侧冲积扇相及扇前河流相,并由后者构成含煤沉积旋回单元的主体;在盆缘断裂活动使得盆缘地带可容空间与沉积物体积相匹配的条件下,形成盆缘断裂内侧冲积扇后,很少有较粗碎屑向更远处进积,扇前大面积泥炭沼泽化形成了含煤沉积旋回单元的顶部煤层。上述两种情况周期性交替形成了铁法盆地的含煤沉积旋回。   相似文献   

东昆仑小庙基性岩脉地球化学及LA-ICP-MS锆石U-Pb定年   总被引：5，自引：0，他引：5  

任军虎  柳益群  周鼎武  冯乔  张琨  董忠良  秦萍莉 《吉林大学学报(地球科学版)》2010,40(4):859-868

东昆仑小庙辉绿岩脉侵位于前寒武纪金水口群变质基底中,岩石地球化学研究表明:它是以低TiO₂和较低的MgO,Nb、Ta亏损和Th富集为特征,贫P₂O₅,Na₂O＞K₂O, 富集大离子亲石元素Rb、Ba、Th、U、Sr和LREE,高场强元素分异明显,地壳源区对辉绿岩的影响很大,形成于大陆拉张带或裂谷初期环境。LA-ICP-MS锆石U-Pb同位素定年结果表明:1 996~2 428 Ma年龄可能代表岩浆捕获锆石年龄,形成于太古宙至古元古代的区域性构造热事件;3个较一致点的加权平均年龄（733.6±6.6） Ma（MSWD =0.038）为辉绿岩结晶年龄,可能代表了新元古代东昆仑地区裂解的时间,这与Rodinia超大陆裂解相对应。  相似文献   

下扬子区海相中、古生界地质结构分区及其油气勘探选区意义   总被引：1，自引：1，他引：0  

李亚辉  段宏亮  谈迎 《地质力学学报》2010,16(3):271-280

基于对下扬子区海相中、古生界构造及沉积沉降特征的研究, 以影响和反映构造稳定及晚期生烃的基底性质、构造变形特征、印支面埋深、沉积沉降中心迁移特征等为依据, 将下扬子区划分为5个一级、17个二级地质结构区。以构造稳定、有效保存及晚期生烃、晚期成藏等为评价标准, 综合评价南黄海中部晚期隆起稳定区(Ⅰ₂)、江都-东台-南黄海南部晚期沉降深冲断区(Ⅰ₃)、泰兴-海安晚期沉降深冲断区(Ⅱ₁)、南通-南黄海南部晚期沉降浅推覆区(Ⅱ₂)及太湖晚期沉降浅推覆区(Ⅱ₄)为下古生界油气勘探有利区; 南黄海北部晚期沉降深冲断区(Ⅰ₁)、江都-东台-南黄海南部晚期沉降深冲断区(Ⅰ₃)、滨海-大丰晚期沉降深下古卷入区(Ⅰ₄)和泰兴-海安晚期沉降深冲断区(Ⅱ₁)为上古生界油气勘探有利区; 南黄海北部晚期沉降深冲断区(Ⅰ₁)、滨海-大丰晚期沉降深下古卷入区(Ⅰ₄)、金湖-高邮晚期沉降深下古卷入区(Ⅰ₅)及泰兴-海安晚期沉降深冲断区(Ⅱ₁)为古潜山油气勘探有利区。研究对于该区海相中古生界勘探选区具有重要意义。   相似文献   

东海盆地西湖凹陷构造样式及其演化     

宋小勇  储呈林  芮志峰 《高校地质学报》2010,16(1):86-93

西湖凹陷是经历多期构造作用的白垩—第三纪盆地。多期裂陷和反转构造作用的叠加导致了相对复杂的构造格架样式和盆地地质结构。凹陷总体上具有东西分带,南北分块的构造格局。裂陷期的同沉积断裂组成了多种复合的构造样式：西部斜坡带主要发育断阶、地堑和地垒构造;中央洼陷带则以复合“Y”字型、羽状和似花状断裂组合为主;东缘断阶带主要发育“Y”字型、梳状和羽状组合。坳陷反转期,早期的同沉积断裂发生了不同程度的逆冲反转,形成了多种复合的构造样式,例如反冲叠瓦扇构造、后断叠瓦式逆冲构造等叠合构造样式。从盆地的构造样式出发,探讨了盆地的形成演化和构造- 沉积充填过程对有利圈闭带发育分布的控制作用,对富生烃凹陷油气预测具有重要指导意义。  相似文献   

Geography and Rural Household Income： A Village Level Study in Henan Province, China   总被引：2，自引：0，他引：2  

Xiaojian Li  Xinsheng Fan 《中国地理科学(英文版)》2010,20(1):1-8

This study uses the data from a sample survey conducted in April 2007 on 1 251 rural households in 11 villages of Henan Province, the largest less developed agricultural province in China, to examine how geography affects rural household income (RHI). The quantitative analysis indicates following results. 1) The significance of the traditional geographical factors reduces as RHI rank increases. 2) The landform does not affect the RHI significantly. The per capita income of rural household in a plain area is lower than that in a mountainous area. And 3) the capital endowment and status of non-farm economic activities contribute to the increase of RHI. But the probability and intensity of non-farm economic activities of rural households in urban outskirts villages are higher than that in non-urban outskirts villages. Based on the results, the paper further concludes that geography still plays a significant role in rural development, but it is changing over time. The agricultural resources (such as per capita arable land) significantly affect RHI with the relatively lower income level, while the geographical location shows a more significant impact on RHI with the relatively high income level. Along with economic development, the proximity replaces the traditional geographical factors such as landform and physical resources as the major determining factor in RHI.  相似文献   

Quantitative Assessment of Impacts of Regional Climate and Human Activities on Saline-alkali Land Changes： A Case Study of Qian＇an County, Jilin Province     

LIAN Yi  WANG Jie  TU Gang  REN Hongling  SHEN Baizhu  ZHI Keguang  LI Shangfeng  GAO Zongting 《中国地理科学(英文版)》2010,20(1):91-97

Interdecadal and interannual variations of saline-alkali land area in Qian’an County, Jilin Province, China were comprehensively analyzed in this paper by means of satellite remote sensing interpretation, field flux observations and regional climate diagnosis. The results show that on the interannual scale, the impact of climate factors accounts for 71.6% of the total variation of the saline-alkali land area, and that of human activities accounts for 28.4%. Therefore the impact of climate factors is obviously greater than that of human activities. On the interdecadal scale, the impact of climate factors on the increase of the saline-alkali land area accounts for 43.2%, and that of human activities accounts for 56.8%. The impact of human activities on the variation of saline-alkali land area is very clear on the interdecadal scale, and the negative impact of human activities on the environment should not be negligible. Besides, changes in the area of heavy saline-alkali land have some indication for development of saline-alkali land in Qian’an County.  相似文献   

A new carbon and oxygen balance model based on ecological service of urban vegetation   总被引：2，自引：1，他引：1  

Kai Yin  Qianjun Zhao  Xuanqi Li  Shenghui Cui  Lizhong Hua  Tao Lin 《中国地理科学(英文版)》2010,20(2):144-151

The application of human induced oxygen consumption and carbon emission theory in urban region was summed up and on this base a new model of urban carbon and oxygen balance (UCOB) was constructed by calculating the carbon and oxygen fluxes. The purpose was to highlight the role of vegetation in urban ecosystems and evaluate the effects of various human activities on urban annual oxygen consumption and carbon emission. Hopefully,the model would be helpful in theory to keep the regional balance of carbon and oxygen,and provide guidance and support for urban vegetation planning in the future. To test the UCOB model,the Jimei District of Xiamen City,Fujian Province,China,a very typical urban region,was selected as a case study. The results turn out that Jimei′s vegetation service in oxygen emission and carbon sequestration could not meet the demand of the urban population,and more than 31.49 times of vegetation area should be added to meet the whole oxygen consumption in Jimei while 9.60 times of vegetation area are needed to meet the carbon sequestration targets. The results show that the new UCOB model is of a great potential to be applied to quantitative planning of urban vegetation and regional eco-compensation mechanisms.  相似文献   

山西地区小震活动年频次分布特征研究     

梁向军  张蕙 《山西地震》2010,(2):1-7

对山西地区1970年至2008年的小震年频次分布用Klomogorov-Smirnov分布检验法进行检验,得出,山西地区的年频次累计次数与年频次有类似G-R的关系;由年频次分布随时间的变化关系分析,山西带及其北、中、南三个区域在中强震前,小震年频次的峰度、偏度、标准差、CV值、bm值等统计函数均表现出明显的变化。  相似文献   

以2008年汶川8.0级地震为例分析地震触发的静态库仑应力计算的不确定性   总被引：1，自引：1，他引：0  

王力伟  陈棋福 《中国地震》2010,26(3)

人们常用地震产生的静态库仑应力变化解释地震的空间迁移和余震的空间分布规律,但是,在计算静态库仑应力场时,室内试验数据和观测资料往往无法对计算所涉及的参数进行足够的约束,而参数取值的不确定性会直接影响到静态库仑应力的计算结果。不同研究组得到的汶川地震产生的静态库仑应力变化结果并不一样,为研究不同计算模型和参数的选取对静态库仑应力计算的影响,我们通过建立模型并依次改变参数,分析比较了各个参数对计算结果的影响。结果表明:重力、接收断层位置和走向等的影响较小,其他参数均会对静态库仑应力变化量值和符号造成不同程度的影响,其影响在地震破裂面周边尤其明显,计算时参数敏感性分析不可忽略。  相似文献   

南海北部第四系厚度分布图的编制与简要说明     

任镇寰  杨廉法  李春初  王文介 《华南地震》2010,30(3):37-41

收集南海北部大量多道地震和钻井资料,编制了该区域首幅第四系厚度分布图。第四系等厚线总体呈NEE向,特别是珠江口外大陆架最明显,莺歌海、琼东南呈NW-EW-NE向弧形,珠江口大陆架南部存在次一级NW向等厚线。第四系等厚线分布形态明显受到断裂构造控制。  相似文献