青海锡铁山矿区滩间山群新认识   总被引：4，自引：0，他引：4  

樊俊昌  李峰 《地质与勘探》2006,42(6):21-25

锡铁山滩间山群是重要的含矿火山-沉积建造.基于野外地质特征、古生物组合、同位素年龄、构造-热事件和火山-沉积演化等的综合分析,文章认为滩间山群形成于早-晚奥陶世,并重新厘定了4个(构造-)岩石地层单位.新建层序反映柴北缘早古生代经历了大陆裂谷开合演化过程.  相似文献   

Glacial atmospheric CO_2 decline in association with decrease of marine sedimentary phosphorus     

WENG Huanxin  ZHANG Xingmao  WU Nengyou  WANG Ying  CHEN Lihong  ZHONG Hexian  QIN Yachao 《中国科学D辑(英文版)》2006,49(3)

Since the discovery from the ice-core record of South Pole revealed that atmospheric concentration of CO2 of the last glacial was 80―100 ppm less than that of Holocene[1], many researchers[2―6] have obtained a series of important findings to seek the dominant fac- tors controlling its change from marine physical, chemical and biological processes, among which the view has gained increasing attention that phosphorus, as a macronutrient, is a crucial limitation to marine primary production, a…  相似文献   

To the problem of the Oligocene-Miocene boundary position in the northern Caucasus (in support of the Caucasian regional stage)     

E. V. Beluzhenko  E. I. Kovalenko 《Stratigraphy and Geological Correlation》2006,14(2):211-218

Stratigraphic position of the Oligocene-Miocene (Paleogene-Neogene) boundary in the northern Caucasus and, in this connection, of the Alkun Formation and the Caucasian regional stage in geological sections of Maikop deposits, primarily in those of the Belaya and Kuban rivers, is considered. Arguments in support of the Caucasian regional stage are presented and necessity of distinguishing the Karadzhalganian regional stage is called in question. Stratigraphic implications of the Alkun Formation, the regional reference horizon traceable in many sections of the northern Caucasus, are discussed. It is substantiated based on nannoplankton, dinocysts, foraminifers, and distinctive lithological features of deposits that the Oligocene-Miocene boundary is confined to the Alkun Formation at the Belaya River.  相似文献   

青藏高原北部不同地区河流和湖岸阶地的演化特征   总被引：1，自引：0，他引：1  

赵振明  李荣社 《地质通报》2006,(Z1)

把青藏高原北部空白区已完成的1∶25万区调成果报告中有关河流和湖岸地貌的剖面、实测数据提炼出来,将其位置点绘于同一张水系分布图上,然后根据不同位置、不同的剖面、不同的测试数据进行区域性对比研究,结果表明:①青藏高原北部昆仑山中部和东部地区,河谷、湖岸地貌都具有100kaBP、10kaBP、5～6kaBP的阶地,这3个时期东西部河谷、湖岸地貌的形成具有同步性;②昆仑山中部地区具有70kaBP的阶地,昆仑山东部地区具有50kaBP的阶地,这2个时期昆仑山东西部河流、湖岸地貌的形成不具有同步性。对该地区河流、湖岸地貌成因分析后认为,除气候作用外,河流阶地、湖岸阶地对高原北部的隆升具有一定的指示作用,表现为从西向东抬升速率逐渐减小,总体上同一地方从老到新抬升速率逐渐增加。  相似文献   

鲁北济阳坳陷东营凹陷南坡沙河街组第四段上亚段高分辨率层序地层格架     

戴朝强  张金亮 《地质通报》2006,(Z2)

应用高分辨率层序地层学与沉积学等理论,通过对地震、录井、测井资料的分析,对鲁北东营凹陷南坡沙河街组第四段上亚段进行了高分辨率层序地层学的划分与对比,总结出各层序地层单元及其界面在录井和地震资料中的判识标志,把研究区基准面旋回划分为短期、中期和长期3个级别的旋回层序。整个沙河街组第四段上亚段由一个长期基准面旋回组成,并划分出5个中期基准面旋回,首次建立了研究区内该亚段高分辨率层序地层格架,有利于东营凹陷南坡该亚段沉积微相和储层结构描述等精细地质研究的进一步开展。  相似文献   

Sedimentary environments of organic matter from Middle Permian source rocks in northern Xinjiang, China   总被引：3，自引：0，他引：3  

苗建宇寇韩生  周立发韩宗元 《中国地球化学学报》2006,25(3):258-265

1IntroductionThe formation of the Junggar,Turpan and Ili ba-sins is ascribed to Hercynian orogeny between theJunggar and Tianshan Mountains during the MiddlePermian.The rock assemblage of thick and stable sedi-mentary dark muddy shales interbedded with th…  相似文献   

辽河坳陷西部凹陷高升北部地区古近系油气成藏条件分析   总被引：4，自引：0，他引：4  

游国庆  潘家华  张可宝  刘彬  肖开华 《地球学报》2006,27(3):241-246

高升北部地区是渤海湾盆地辽河坳陷重要的油气富集区,正确认识高升北部地区油气成藏条件对于弄清该区的油气分布规律具有重要意义。综合利用地质、地球物理、地球化学和计算机技术对高升北部地区油气成藏的研究表明,高升北部地区具备油气成藏的有利条件,较好的烃源岩经历了有机质的低成熟—成熟演化阶段,扇三角洲前缘砂体是最重要的油气聚集区,储集砂体主要发育在高81井—高70井区带。本区烃源岩有机质的成熟度和储集砂体的发育程度是决定油气藏形成最重要的因素。  相似文献   

Quantitative analysis of the dynamic change and spatial differences of the ecological security: a case study of Loess Plateau in northern Shaanxi Province     

LI Jing  REN Zhiyuan  ZHOU Zixiang 《地理学报》2006,16(2):251-256

Using the theory and method of the ecological footprint, and combining the changes of regional land use, resource environment, population, society and economy, this paper calculated the ecological footprint, ecological carrying capacity and ecological surplus/loss in 1986-2002 on the Loess Plateau in northern Shaanxi Province. What is more, this paper has put forward the concept of ecological pressure index, set up ecological pressure index models, and ecological security grading systems, and the prediction models of different ecological footprints, ecological carrying capacity, ecological surplus and ecological safety change, and also has assessed the ecological footprint demands of 10,000 yuan GDP. The results of this study are as follows: (1) the ecological carrying capacity in northern Shaanxi shows a decreasing trend, the difference of reducing range is the fastest; (2) the ecological footprint appears an increasing trend; (3) ecological pressure index rose to 0.91 from 0.44 during 1986-2002 on the Loess Plateau of northern Shaanxi with an increase of 47%; and (4) the ecological security in the study area is in a critical state, and the ecological pressure index has been increasing rapidly.  相似文献   

Chemical Assessment of Oceanic and Terrestrial Sulfur in the Marine Boundary Layer over the Northern North Pacific during Summer   总被引：2，自引：0，他引：2  

K. Aranami  S. Watanabe  S. Tsunogai  A. Ohki  K. Miura  H. Kojima 《Journal of Atmospheric Chemistry》2002,41(1):49-66

Dimethylsulfide (DMS) in surface seawater and the air, methanesulfonic acid (MSA) and non-sea-salt sulfate (nss-SO₄ ²–) in aerosol, and radon-222 (Rn-222) were measured in the northern North Pacific, including the Bering Sea, during summer (13 July – 6 September 1997). The mean atmospheric DMS concentrations in the eastern region (21.0 ± 5.8 nmole/m³ (mean ± S.D.), n=30) and Bering Sea (19.9 ± 9.8 nmole/m³, n=10) were higher than that in the western region (11.1 ± 6.4 nmole/m³, n=31) (p<0.05), although these regions did not significantly differ in the mean DMS concentration in surface seawater. Mean sea-to-air DMS flux in the eastern region (21.0 ± 10.4 mole/m²/day, n=19) was larger than those in the western region (11.3 ± 16.9 mole /m²/day, n=22) and Bering Sea (11.2 ± 7.8 mole/m²/day, n=7) (p<0.05). This suggests that the longitudinal difference in atmospheric DMS was produced by that in DMS flux owing to wind speed, while the possible causes of the higher DMS concentrations in the Bering Sea include (1) later DMS oxidation rates, (2) lower heights of the marine boundary layer, and (3) more inactive convection. The mean MSA concentrations in the eastern region (1.18 ± 0.84 nmole/m³, n=35) and Bering Sea (1.17 ± 0.87 nmole/m³, n=13) were higher than that in the western region (0.49 ± 0.25 nmole/m³, n=28) (p < 0.05). Thus the distribution of MSA was similar to that of DMS, while the nss-SO₄ ²– concentrations were higher near the continent. This suggests that nss-SO₄ ²– concentrations were regionally influenced by anthropogenic sulfur input, because the distribution of nss-SO₄ ²– was similar to that of Rn-222 used as a tracer of continental air masses.  相似文献   

Atmospheric Mercury Concentrations from Several Observatory Sites in the Northern Hemisphere   总被引：4，自引：0，他引：4  

Ki-Hyun?KimEmail author  R.?Ebinghaus  W.?H.?Schroeder  P.?Blanchard  H.?H.?Kock  A.?Steffen  F.?A.?Froude  Min-Young?Kim  Sungmin?Hong  Jae-Hwan?Kim 《Journal of Atmospheric Chemistry》2005,50(1):1-24

In an effort to investigate both large-scale (spatial) and short/long-term (temporal) distribution characteristics of atmospheric mercury, we have combined and analyzed the Hg concentration data sets collected continuously by four different scientific groups for the areas and periods covering (1) America (three sites near the Canadian Great Lakes (CGL): 1997–2000), (2) Asia (Seoul, Korea (SEL): 1997–2002), (3) Arctic (Alert, Canada (ALT): 1995–2001), and (4) Europe (Mace Head, Ireland (MH): 1996–2002). The mean concentrations of Hg data from those widely dispersed monitoring stations were computed to be (1) 1.58 ± 0.23, 1.69 ± 0.32, and 1.93 ± 0.44 (three sites in CGL), (2) 5.06 ± 2.46 ng m^–3 (SEL), (3) 1.55 ± 0.41 (ALT), and (4) 1.76 ± 0.31 (MH). Intersite relationships were investigated among all different stations using the data groups divided into different temporal intervals. The analysis of diurnal variation patterns of Hg indicated differences in regional source/sink characteristics, with increasing amplitudes of variability toward areas under the strong influence of anthropogenic sources. When the analysis was made over different seasons, the patterns contrasted greatly between the Arctic and the other areas. It was found that the relative enhancement of Hg concentrations was dominant during winter/spring in most areas due to direct or indirect influences of anthropogenic emissions. However, the pattern for the Arctic area was distinguished pronouncedly from others with the spring minimum and summer maximum both of which reflect the potent effects of mercury depletion phenomenon (MDP). By contrast, no long-term trend, either being an increase or decrease, was evident from any of the stations during each respective study period. Although our initial attempts to examine the distribution characteristics of Hg analyzed by different scientific groups were successful, we feel that these efforts should be continued further to extend the compatibility of the global database of Hg.  相似文献