Monitoring periodically national land use changes and analyzing their spatiotemporal patterns in China during 2015–2020     

Kuang  Wenhui  Zhang  Shuwen  Du  Guoming  Yan  Changzhen  Wu  Shixin  Li  Rendong  Lu  Dengsheng  Pan  Tao  Ning  Jing  Guo  Changqing  Dong  Jinwei  Bao  Yuhai  Chi  Wenfeng  Dou  Yinyin  Hou  Yali  Yin  Zherui  Chang  Liping  Yang  Jiuchun  Xie  Jiali  Qiu  Juan  Zhang  Hansong  Zhang  Yubo  Yang  Shiqi  Sa  Rigai  Liu  Jiyuan 《地理学报(英文版)》2022,32(9):1705-1723

Journal of Geographical Sciences - High-resolution mapping and monitoring of national land use/cover changes contribute significantly to the knowledge of the interaction between human activities...  相似文献   

北淮阳地区变质地层序列与构造变形特征   总被引：18，自引：0，他引：18  

汤加富  侯明金  石乾华  周存亭  徐家聪 《安徽地质》1995,(3)

本文较详细阐述了近年来北淮阳地区在变质地层序列与构造变形特征方面研究的新进展。对梅山群的解体与新归属、原庐镇关群的解体与废名、佛子岭岩群的新含义作了简要论述。通过近年来不断深入的构造解剖，阐明了区内由早期伸展构造体制下的褶叠层；主期收缩体制下，以折劈理为标志的叠加向斜；以及晚期多期次自南而北的滑覆逆冲构造的主要特征，将为区内在新的地质背景下开展找矿工作提供了地质依据。  相似文献   

Listening to the Deep: live monitoring of ocean noise and cetacean acoustic signals     

André M  van der Schaar M  Zaugg S  Houégnigan L  Sánchez AM  Castell JV 《Marine pollution bulletin》2011,63(1-4):18-26

The development and broad use of passive acoustic monitoring techniques have the potential to help assessing the large-scale influence of artificial noise on marine organisms and ecosystems. Deep-sea observatories have the potential to play a key role in understanding these recent acoustic changes. LIDO (Listening to the Deep Ocean Environment) is an international project that is allowing the real-time long-term monitoring of marine ambient noise as well as marine mammal sounds at cabled and standalone observatories. Here, we present the overall development of the project and the use of passive acoustic monitoring (PAM) techniques to provide the scientific community with real-time data at large spatial and temporal scales. Special attention is given to the extraction and identification of high frequency cetacean echolocation signals given the relevance of detecting target species, e.g. beaked whales, in mitigation processes, e.g. during military exercises.  相似文献   

Stochastic simulation of bivariate gamma distribution: a frequency-factor based approach     

Ke-Sheng Cheng  Ju-Chen Hou  Jun-Jih Liou  Yii-Chen Wu  Jie-Lun Chiang 《Stochastic Environmental Research and Risk Assessment (SERRA)》2011,25(2):107-122

A frequency-factor based approach for stochastic simulation of bivariate gamma distribution is proposed. The approach involves generation of bivariate normal samples with a correlation coefficient consistent with the correlation coefficient of the corresponding bivariate gamma samples. Then the bivariate normal samples are transformed to bivariate gamma samples using the well-known general equation of hydrological frequency analysis. We demonstrate that the proposed bivariate gamma simulation approach is capable of generating random sample pairs which not only have the desired marginal densities of component random variables but also their correlation coefficient. Scatter plots of simulated bivariate sample pairs also exhibit appropriate linear patterns (dependence structure) that are commonly observed in environmental and hydrological applications. Caution should also be exercised when specifying combinations of coefficients of skewness and the correlation coefficient for bivariate gamma simulation.  相似文献   

西安地区砌体结构校舍抗震加固设计方法研究     

侯卫  周雪峰  郝丽  申建光 《震灾防御技术》2011,6(2):130-135

对震后中小学校舍进行抗震加固是我国各级政府在汶川地震后给工程技术人员提出的重要课题.本文针对西安地区中小学校舍的抗震加固设计进行了论述.对其存在的安全隐患,可依据抗震鉴定的结论及现场实地勘察,综合考虑施工进度、施工复杂程度、工期等因素,选用相应的抗震加固设计方案.根据设计过程中出现的问题,本文还提出了工程建议,可为类似的工程设计、施工提供借鉴.  相似文献   

Gushan magnetite–apatite deposit in the Ningwu basin, Lower Yangtze River Valley, SE China: Hydrothermal or Kiruna-type?     

Tong Hou  Zhaochong Zhang  Timothy Kusky 《Ore Geology Reviews》2011,43(1):333-346

The Gushan deposit is one of the typical magnetite–apatite deposits associated with dioritic porphyries in the Lower Yangtze River Valley belt of the eastern Yangtze craton. The origin of this deposit is still uncertain and remains a controversial issue. Divergent opinions are centered on whether the iron deposits are magmatic or hydrothermal in origin. However, our field observations and mineralogical studies, combined with previous published petrological and geochemical features strongly suggest that the main ore bodies in the Gushan magnetite–apatite deposit are magmatic. Specific evidence includes the existence of gas bubbles, tubes, and miarolitic and amygdaloidal structures, melt flow banding structure and the presence of “ore breccia”. New electron microprobe analyses of the pyroxene phenocrysts of the dioritic porphyry genetically associated with the Gushan magnetite–apatite deposit show that the Fe contents in the evolving magma dramatically decrease, and then gradually increase. Because there is no evidence of mafic magma recharge, this scenario (decreasing Fe) could be plausibly interpreted by Fe-rich melts separated from Fe-poor silicate melts, i.e., liquid immiscibility was triggered by minor addition of phosphorus by crustal contamination. The occurrence of massive iron ore bodies can be satisfactorily explained by the immiscible Fe-rich melt with enormous volatile contents was driven to the top of the magma chamber due to the low density. The hot and volatile-rich iron ore magma was injected along fractures and spaces between the dioritic intrusions and wall-rocks, and led to an explosion near the surface, resulting in the immediate fragmentation of the roof of the intrusion and wall-rocks, forming brecciated ores. Moreover, other types of ores can be considered as a result of post-magmatic hydrothermal activities. Our proposed metallogenic model involving the Kiruna-type mineralization is consistent with the observed phenomenon in the Gushan deposit.  相似文献   

沁水盆地南部变质变形煤储层特征层气富集区划分          下载免费PDF全文

卫明明  琚宜文  薛传东  侯泉林 《地质科学》2011,(3):905-918

沁水盆地南部周缘被挤压性断裂褶皱带所围限,区内缓坡带形成煤层气富集区.受中新生代区域构造—热演化影响,盆地内煤储层在深成变质作用基础上叠加了不同程度的构造动力变质作用和岩浆热变质作用,产生了不同程度的变质和变形,导致其在变质变形程度、含气性及渗透性等煤储层物性方面具有不同的特征,有明显的区域分异,形成展布方向与盆地复向...  相似文献   

高能粒子流对地震活动的可能调制     

罗葆荣 《天文研究与技术》1995,(2)

把地球作为一个开放系统，本文分析了不同地域范围的地震活动和太阳活动的关系，发现不同地域的地震活动也存在着一个大约１１年的周期，这个周期可能与太阳活动的１１年左右周期有关，但地震周期的峰值对应于太阳活动的下降段。它们的关系是负相关关系。本文进一步着重分析了地震活动与高速太阳风粒子流和宇宙线高能粒子流的关系，发现它们之间存在着一个信度水平很高的正相关。这样，我们可以推测太阳活动可能是通过调制到达地球的高能粒子流进而调制地震活动的。  相似文献   

北山造山带古生代浊积岩构造环境探讨及其大地构造意义   总被引：1，自引：0，他引：1       下载免费PDF全文

郭谦谦  肖文交  侯泉林  韩春明  曲军锋  田忠华  宋东方 《地质科学》2013,(1):50-70

北山造山带是研究中亚造山带增生造山的关键地区之一,浊积岩是增生造山带的重要组成部分。北山古生代浊积岩主要出露于营毛沱、柳园和黑山口地区。营毛沱浊积岩发育于下奥陶统,古水流方向由南向北,内部砂岩具中高等风化程度的长英质源区,构造背景为被动陆缘。早二叠世柳园浊积岩内部砂岩具低到中等风化程度的中基性源区,构造背景为大洋岛弧。早二叠世黑山口浊积岩中的砂岩源区具中等风化程度,环境相对柳园砂岩较为稳定,和长英质源区的沉积岩具相似性,构造环境可能为活动陆缘弧。对北山古生代浊积岩的解剖揭示北山古生代经历了复杂的俯冲增生过程。早古生代花牛山-火石山一带发育向北的俯冲,火石山南部被动陆缘形成营毛沱浊积岩,之后的俯冲带局部后撤形成泥盆纪墩墩山岛弧。柳园地区晚古生代洋壳向花牛山和石板山岛弧带俯冲分别形成了柳园和黑山口浊积岩。本研究支持北山增生时间持续到早二叠世的观点,对认识天山、索伦缝合带的衔接对比研究具有重要的意义。  相似文献   

孔隙结构对低渗-特低渗砂岩储层渗流特征的影响段储层为例——以鄂尔多斯盆地东部上古生界盒8段储层为例   总被引：1，自引：0，他引：1       下载免费PDF全文

李杪  罗静兰  刘新社  赵会涛  王怀厂  侯云东 《地质科学》2013,48(4):1148-1163

通过铸体薄片显微镜下观察、孔喉图像、毛细管压力、恒速压汞、气水相对渗透率、核磁共振等多种分析实验手段,研究了鄂尔多斯盆地东部上古生界盒8段低孔、低渗-特低渗砂岩储层的微观孔隙结构和渗流特征,探讨了孔隙结构对储层渗流特征的影响。结果表明,孔隙结构特征是影响低孔、低渗-特低渗砂岩储集性能与渗流特征的主要因素。而砂岩的孔隙结构特征主要受砂岩原生矿物组合与成岩演化过程及其产物的控制,盒8段各砂岩类型由于其矿物成分不同导致孔隙结构的差异,也是各砂岩类型储集性能与渗流能力存在差别的直接原因。在孔隙结构参数中,喉道的大小、有效孔隙与喉道的体积及其连通性是决定储层储集与渗流能力的关键。大孔喉对储层渗流能力的贡献更大,中-小孔喉则对储集能力的贡献相对较高。微裂缝是除孔隙结构以外影响砂岩储集性能与渗流特征的重要因素。  相似文献