Structural Evolution of the Eastern Qiulitagh Fold and Thrust Belt,Northern Tarim Basin,China   总被引：4，自引：3，他引：1  

YANG Minghui  JIN Zhijun  LU Xiuxiang  SUN Dongsheng  TANG Xuan  PENG Gengxin  LEI Ganglin 《《地质学报》英文版》2009,83(2):347-358

The eastern Qiulitagh fold and thrust belt (EQFTB) is part of the active Kuqa fold and thrust belts of the northern Tarim Basin. Seismic reflection profiles have been integrated with surface geologic and drill data to examine the deformation and structure style of the EQFTB, particularly the deformational history of the Dina 2 gas field. Seismic interpretations suggest that Dongqiu 8 is overall a duplex structure developed beneath a passive roof thrust, which generated from a tipline in the Miocene Jidike Formation, and the sole thrust was initiated from the same Jidike Formation evaporite zone that extends westward beneath the Kuqatawu anticline. Dongqiu 5 is a pop-up structure at the western part of the EQFTB, also developed beneath the Jidike Formation evaporite. Very gentle basement dip and steep dipping topographic slope in the EQFTB suggest that the Jidike Formation salt provides effective decoupling. The strong deformation in the EQFTB appears to have developed further south, in an area where evaporite may be lacking. Since the Pliocene, the EQFTB has moved farther south over the evaporite and reached the Yaken area. Restoring a balanced cross-section suggests that the minimum shortening across the EQFTB is more than 7800 m. Assuming that this shortening occurred during the 5.3 Ma timespan, the shortening rate is approximately 1.47 mm/year.  相似文献   

基于凸壳构造技术的领海基点选取问题研究   总被引：8，自引：0，他引：8  

彭认灿  王家耀  田震  郭立新  陈子澎 《测绘学报》2005,34(1):53-57

领海基点的选取数量及其空间点位分布的不同,对海域划界结果有着重要的影响.在传统的领海基点选取工作中缺乏一种有效的用于检验选取方案优劣的数学模型,因而这一工作中存在着不确定性因素.为了解决这个问题,提出了利用最小凸包(凸壳)构造技术实现领海基点最优选取的思路和方法,并在此基础上对某群岛的领海基点选取方案作了实例分析.  相似文献   

洞庭湖区生态承载力时空演化特征   总被引：4，自引：0，他引：4  

熊建新  彭保发  陈端吕 《地理研究》2013,32(11):2031-2040

利用探索性空间数据分析以及百分位数和变异系数,基于Arc GIS 和Geo DA软件支撑,对洞庭湖区生态承载力的空间格局特征、空间关联特征和相对差异演变特征进行分析。结果表明：① 空间格局上,洞庭湖区生态承载力从西南向东北大体上呈现“W”型（较高—低—高—低—较高）空间格局,倒“U”型的县域差异特征显著。② 空间关联上,洞庭湖区生态承载力的分布呈正的全局空间自相关,出现相似县域之间的空间集聚,全局Moran’s Ⅰ值相差不大,空间聚集程度比较稳定,趋于围绕某一偏低集聚度出现小范围内波动;局部空间自相关的LISA 集聚类型出现HH型、HL型和LH型3 种类型,依次集中分布在洞庭湖区的中部、西南部和东北部,局部空间格局保持相对稳定,但是聚类特征显现出稍微变化的迹象。③ 相对差异演变上,2001-2010 年洞庭湖区生态承载力相对差异演变整体上呈现一定的差异性。2001-2003 年相对差异较小,趋于稳定;2005 年前后相对差异较大;相比2001-2003 年,2005 年以来相对差异明显扩大且这种较大的空间相对差异随着时间的推移呈现小幅波动趋势。  相似文献   

硫酸镁对硼酸介稳区性质的影响   总被引：2，自引：1，他引：1       下载免费PDF全文

李丽丽  董亚萍  彭姣玉  李武  孟庆芬 《盐湖研究》2013,21(1):38-43

通过浊度法测定10℃～45℃范围内MgSO4-H3BO3-H2O体系中硼酸的溶解度及介稳区宽度,得到硼酸的成核方程,并计算其表观成核级数。实验结果表明,硫酸镁的存在降低了硼酸的溶解度;随着硫酸镁浓度的升高,硼酸的介稳区宽度先变宽后变窄;硫酸镁的加入使硼酸的表观成核级数增加。  相似文献   

三江并流区云南贡山片植被景观类型分布特征   总被引：1，自引：0，他引：1  

欧光龙  彭明春  王崇云  向伶 《山地学报》2013,31(4):464-472

以三江并流区云南贡山片为例,以Landsat ETM+影像为数据源,基于3S技术进行植被景观制图,分析景观类型的分布特征。结果表明:1.研究区是典型的高山峡谷地区,海拔3 000~4 000 m的区域占总面积近一半,坡度25°以上的山地面积占84.82%;景观类型分布受垂直空间分异主导;河流、河漫滩和湖泊等景观主要分布在平缓地段,自然植被景观多分布在25°~45°的陡坡上,人工植被景观分布的坡度范围相对较缓;自然植被景观在各坡向上的分布较为均匀;人工植被景观及积雪/冰川景观、岩石景观等分布则体现出一定的空间分异;2.山地森林植被构成研究区景观的基质类型;由于植被景观的垂直分异,构成基底的各类景观类型的优势度随海拔变化,河谷地段的中山湿性常绿阔叶林、中山-亚高山的铁杉-常绿阔叶混交林、亚高山-高山的云冷杉/落叶松林优势度较高,高山-亚高山以杜鹃灌丛为优势景观类型;3.从斑块粒度上看,小斑块数量最多,占总斑块数的80.87%,中斑块占11.36%,其余均在3%以下;优势自然景观类型具有较大的巨斑块数;巨斑块面积比例最大,达到68.99%,其余斑块大小等级的分布面积比例在3%~9%之间。  相似文献   

Transcriptional response of Microcystis aeruginosa to the recruitment promoting-benthic bacteria     

Juan WANG  Yuande PENG  Zhi WANG  Wansheng ZOU  Xianjin PENG  Qisheng SONG 《海洋湖沼学报（英文）》2022,(1):153-162

Blooms of Microcystis aeruginosa occur frequently in many freshwater ecosystems around the world, but the mechanism of recovery has not been fully understood. I...  相似文献   

Using live vegetation volume to analyze the effects of plot Pinus massoniana Lamb on water and soil conservation under natural rainfall events   总被引：1，自引：0，他引：1  

Zhu-jun GU  Xiao-xia WU  Xiao-lei WANG  Shao-yun PENG  Hao LUO  Xue-zheng SHI  Dong-sheng YU 《国际泥沙研究》2013,28(4):579-587

The 3-D spatial distributions of vegetation are of great significance for water and soil conservation but are rarely concerned in literatures. The live vegetation volume （LVV） was used to relate to water/soil loss under 144 natural erosive rainfall events from 2007 to 2010 in a typical water-eroded area of southern China. Quadratic polynomial regression models were established for five pure tree （Pinus massoniana Lamb） plots between LVV and water （rtmoff）/soil conservation effects （RE/SE）. RE/SE corresponds to the ratios of runoff depth/soil loss of the pure tree plots to that of the control plot under each rainfall event. Increasing LVV exhibits descending （DS）, descending-ascending （DA）, ascending-descending （AD）, and ascending （AS） trends in the LVV-RE and LVV-SE curves. The effects of soil conservation on the plots were generally more noticeable than the effects of water conservation, and most of the RE and SE values reflected the positive effects of water and soil conservation. The effects were mainly positive under heavy rains （e.g., rainfall erosivity, R = 140 MJ mm ha-l h, maximum 30 min intensity, I30 = 16 mm h-l）, whereas the effects were mainly negative under light rains （e.g., R = 45 MJ mm ha-1 h, I30 = 8 mm h-l）. The trees＇ water/soil conservation effects notably transformed when rainfall erosivity and intensity were lower than the positive or negative effects to a certain threshold. About 50% rainfall events led to obvious transform effects when LVVs were near 0.5 or 0.6. These results are able to aid in the decision making on the forest reconstruction in water-eroded areas.  相似文献   

西藏打加错南北向地堑系的形成特征及其与成矿的关系     

龚臣  彭建华  黄韶春  赵希良 《火山地质与矿产》2013,(4):249-256

西藏打加错南北向地堑系处于冈瓦纳大陆北缘,地堑系总体延伸方向（175～190°）,延伸长度＞50 km,延伸宽度5～15 km.根据该地堑构造带内发育的鱼鳞山组（N2Qy）玄武岩测年结果以及地堑构造带内发育的活动温泉,判断该地堑构造活动时期早于13.43 Ma,现今仍在强烈活动.在打加错地堑系东西两侧的地垒中共发现5处金属矿（化）点,各矿（化）点与中酸性岩体活动及近SN断裂构造有密切关系,特别是近南北向展布的中酸性小岩体更易形成斑岩型铜矿.  相似文献   

Retrieval algorithm for microwave surface emissivities based on multi-source, remote-sensing data: An assessment on the Qinghai-Tibet Plateau   总被引：1，自引：0，他引：1  

WANG YongQian  SHI JianCheng  LIU ZhiHong  PENG YingJie  LIU WenJuan 《中国科学:地球科学(英文版)》2013,(1):93-101

The Qinghai-Tibet Plateau plays a very important role in studying severe weather in China and around the globe because of its unique characteristics. Moreover, the surface emissivities of the Qinghai-Tibet Plateau are also important for retrieving surface and atmospheric parameters. In the current study, a retrieval algorithm was developed to retrieve the surface emissivities of the Qinghai-Tibet Plateau. The developed algorithm was derived from the radiative transfer model and was first validated using simulated data from a one-dimensional microwave simulator. The simulated results show good precision. Then, the surface emissivities of the Qinghai-Tibet Plateau were retrieved using brightness temperatures from the advanced microwave-scanning radiometer and atmospheric profile data from the moderate resolution imaging spectroradiometer. Finally, the features of the time and space distribution of the retrieved results were analyzed. In terms of spatial characteristics, a spatial distribution con- sistency was found between the retrieved results and surface coverage types of the Qinghai-Tibet Plateau. In terms of time characteristics, the changes in emissivity, which were within 0.01 for every day, were not evident within a one-month time scale. In addition, surface emissivities are sensitive to rainfall. The reasonability of the retrieved results indicates that the algorithm is feasible. A time-series surface emissivity database on the Qinghai-Tibet Plateau can be built using the developed algorithm, and then other surface or atmospheric parameters would have high retrieval precision to support related geological re- search on the Qinghai-Tibet Plateau.  相似文献   

抑螺防病林建设中生物材料的筛选及抑螺机理研究进展   总被引：1，自引：0，他引：1  

孙启祥  彭镇华 《湿地科学与管理》2013,(3):8-11

血吸虫病是一种严重危害人们身体健康的重大传染病,林业血防生态工程建设是防治血吸虫病的有效手段,生物材料的筛选是林业血防建设的重要环节。阐述了抑螺防病林建设中生物(植物、微生物)材料筛选及研究进展,并从钉螺生理响应和解剖结构等方面系统分析了生物材料抑螺机理。  相似文献