Early Permian Conodonts from the Baoshan Block, Western Yunnan, China   总被引：3，自引：0，他引：3  

JI Zhansheng  YAO Jianxin  JIN Xiaochi  YANG Xiangning  WANG Yizhao  YANG Hailin  WU Guichun Institute of Geology  Chinese Academy of Geological Sciences  Baiwangzhuang Ro  Beijing  Department of Earth Sciences  Nanjing University  Nanjing  Jiangsu Geological Survey of Yunnan  Yujiang Ro  Yuxi  Yunnan 《《地质学报》英文版》2004,78(6):1179-1184

The Rabeignathus bucaramangus fauna was recently found from the limestone beds of the top part of the elastics-dominated Dingjiazhai Formation in the Aluotian section, southern Baoshan Block, western Yunnan. With Rabeignathus bucaramangus as the dominant species, this fauna includes Rabeignathus bucaramangus (Rabe), Homeoiranognathus huecoensis (Ritter), Sweetognathus inomatus Ritter, Sweetognathus whitei (Rhodes), Mesogondolella cf. bisselli (Clark and Behnken) and a few of ramiform elements. The characteristies of the fauna suggest that it can be correlated with the upper part of the Sweetognathus whitei Zone and assigned to the Middle Artinskian.  相似文献   

ESR Dating of the Evolution of the Shuanghu Basin in the Northern Tibetan Plateau   总被引：3，自引：0，他引：3  

WU Zhenhan  JIANG Wan  Peter Blisniuk  BI Siwen  ZHANG Shukun  Olaf Kuchel  MAO Yi Institute of Geomechanics  CAGS  Minzu Xueyuan Nanlu  Beijing Institut fur Geowissenschaften  Universitat Potsdam  Postfach  D- Potsdam  Germany Liu Xinzhu 《《地质学报》英文版》1999,73(3):289-293

The Shuanghu basin is a NE-trending rift basin bounded by NE-striking normal faults and NW-striking shear-extensional faults of the northern Tibetan Plateau. Four samples from calcite veins in marginal faults and one sample from mudstone (S-3) were collected for dating the evolution of the Shuanghu basin by using the ESR spectrograph of EXM-type. Ages were calculated according to the close-equilibrium model on the basis of the measured ESR signal spectra of samples, providing good chronological information. It is known from the ESR dating that the extensional faulting and rifting of the Shuanghu area began at 4.92 Ma B.P., followed by regional folding in 3.56-1.36 Ma, NW-striking faulting in 0.60 Ma and normal faulting in 0.024 Ma in the Shuanghu basin.  相似文献   

成都平原传统场镇与林盘居民点的分布特征及其影响因素——以成都郫县为例     

黄学渊  张蕾  周莲 《热带地理》2020,40(5):856-867

基于近现代地图与相关地理信息,结合历史文献与实地考察,通过GIS空间分析、核密度估算、欧氏距离、基尼系数等方法,以传统林盘聚落的核心区成都郫县为例,定量揭示了1947、1970、1985、2000与2018年郫县林盘居民点的空间分布特征与场镇分布关系的变化情况。结果表明：1）不同时期林盘居民点的分布具有明显的空间差异性,在改革开放前,林盘居民点的分布极易受到政治经济中心的影响,在改革开放后,其具有均质化快速发展的特点,但城镇化的快速推进从根本上改变了林盘居民点的散居特征,其聚集程度明显增高。林盘居民点高密度区始终具有围绕传统场镇及城镇建成区分布的特点。2）传统场镇的市场半径大致为3 km,交通条件是其选址的首要因素,民国时期场镇选址主要受水路交通影响,建国后水路交通为场镇带来的交通便利逐渐被陆路交通所取代。3）传统场镇的分布会随着林盘居民的自组织行为与相关政策的调控而不断趋于均衡状态,但在改革开放之后,场镇由乡村市场驱动的自由放任式发展转变为地方政府驱动下的固定场所。4）林盘居民点具有沿河流水系分布的特点;传统时期林盘居民点与主要道路之间的关联性较低,但当前其具有沿道路分布的特点。  相似文献   

Analysis of the vertical temperature distribution of shallow snow layers near Taishan Station,East Antarctica          下载免费PDF全文

Zhang Yuzhong  Tang Xueyuan  Dou Yinke  Guo Jingxue  Zuo Guangyu 《极地研究》1988,31(4):413

  相似文献   

Chaos Dynamic Behaviour of Mineralization     

MA Tuhu  ZHU Xingsheng  LI Changjiang Institute of Geology  Mineral Resources of Zhejiang Province  Tiyuchang Ro  Hangzhou 《《地质学报》英文版》1998,72(4):392-398

In this paper a nonlinear dynamic model for the distribution of element content and mineralization in the crust is suggested and the iteration relationship formula of this model coincides with the logistic equation. This shows that mineralization related with migration and enrichment of elements is in chaos, thus resulting in fractal structures of element content and ore reserves and their spatial distribution in the crust.  相似文献   

Oncolites of the Lower Permian ChuanshanFormation in South China and Their Geologicaland Economic Significance     

JIANG Yuehu  YUE Wenzhe  YE ZhizhengNanjing Institute of Geology  Mineral Resources  East Zhongshan Ro  Nanjing 《《地质学报》英文版》1998,72(4):441-454

A large amount of oncolites popularly named " Chuanshan balls" occur universally in the Lower Permian Chuanshan Formation in South China. These kinds of oncolites have the following characteristics: wide distribution, huge quantities, large sedimentary thickness and similar characters, which constitute a specific " fashion fades" in geological history. The authors consider that these kinds of oncolites were due to the intense differentiation of the global climate at that time, which resulted in a universal descent of the sea level and breeding of a large amount of algae in sea water over low-latitude areas. According to the distribution and characteristics of the oncolitic, relative relationships between different tectonic blocks may be inferred, diagenetic strength indicated and diagenetic history recovered, and more important, oncolites serve as a favourable reservoir rock, so their study is of great theoretical and economic significance.  相似文献   

Distribution of Carbon and Oxygen Isotopes in theSequence Stratigraphic Framework of the Middle andUpper Proterozoic in the Ming Tombs Area, Beijing     

LI Rufeng University of Petroleum  Shuiku Ro  Changping  Beijing Liu Xinzhu 《《地质学报》英文版》1998,72(2):207-216

This paper discusses the distribution pattern and geological significance of the carbon and oxygen isotopes (δ13C and δ18O) in the depositional sequences of Gaoyuzhuangian, Yangzhuangian and Wumishanian ages of the established Middle and Upper Proterozoic sequence stratigraphic framework in the Ming Tombs area lying in western Yanshan Mountain of Beijing. Besides, sketchy determination of δ13C and δ18O was also performed for other formations and members. The analytical results show the following: under the condition of clear-water carbonate sediments, δ13C and δ18O, featuring smaller variation of δ13C but larger variation of δ18O, can well delineate the relative change of sea level, which reflects the difference of primary sedimentary settings; in the presence of terrigenous substances, δ13C values vary greatly while δ18O slightly; the carbon and oxygen isotopes show marked changes at sequence boundaries. Besides, particular patterns can be found in regard to the distribution of carbon and oxy  相似文献   

The aerosol radiative effect on a severe haze episode in the Yangtze River Delta   总被引：1，自引：1，他引：0  

Kai Sun  Hongnian Liu  Xueyuan Wang  Zhen Peng  Zhe Xiong 《Acta Meteorologica Sinica》2017,31(5):865-873

Due to increased aerosol emissions and unfavorable weather conditions, severe haze events have occurred frequently in China in the last 10 years. In addition, the interaction between the boundary layer and the aerosol radiative effect may be another important factor in haze formation. To better understand the effect of this interaction, the aerosol radiative effect on a severe haze episode that took place in December 2013 was investigated by using two WRF-Chem model simulations with different aerosol configurations. The results showed that the maximal reduction of regional average surface shortwave radiation, latent heat, and sensible heat during this event were 88, 12, and 37 W m^–2, respectively. The planetary boundary layer height, daytime temperature, and wind speed dropped by 276 m, 1°C, and 0.33 m s^–1, respectively. The ventilation coefficient dropped by 8%–24% for in the central and northwestern Yangtze River Delta (YRD). The upper level of the atmosphere was warmed and the lower level was cooled, which stabilized the stratification. In a word, the dispersion ability of the atmosphere was weakened due to the aerosol radiative feedback. Additional results showed that the PM_2.5 concentration in the central and northwestern YRD increased by 6–18 μg m^–3, which is less than 15% of the average PM_2.5 concentration during the severely polluted period in this area. The vertical profile showed that the PM_2.5 and PM₁₀ concentrations increased below 950 hPa, with a maximum increase of 7 and 8 μg m^–3, respectively. Concentrations reduced between 950 and 800 hPa, however, with a maximum reduction of 3.5 and 4.5 μg m^–3, respectively. Generally, the aerosol radiative effect aggravated the level of pollution, but the effect was limited, and this haze event was mainly caused by the stagnant meteorological conditions. The interaction between the boundary layer and the aerosol radiative effect may have been less important than the large-scale static weather conditions for the formation of this haze episode.  相似文献   

黄河流域能源消费碳排放时空格局演变及影响因素——基于DMSP/OLS与NPP/VIIRS夜间灯光数据     

杜海波  魏伟  张学渊  纪学朋 《地理研究》2021,40(7):2051-2065

科学估算并动态监测长时间序列区域能源消费碳排放发展态势,是制定、实施及评估地区碳减排策略的科学依据和基础保障。基于构建的长时间序列可相互比较的DMSP/OLS与NPP/VIIRS两种夜间灯光数据集,本文模拟了2000—2018年黄河流域能源消费碳排放的时空变化特征,并从流域地理分异的角度对其影响因素进行解析。结果表明：① 2000—2018年黄河流域能源消费碳排放呈现总量不断上升但增长速率下降的态势,整体表现出收敛趋势,但还未达到碳峰值;流域内部碳排放总量呈中游>下游>上游的地理分异特征。② 以黄河干流及主要支流为串联的核心城市形成了若干规模不一的高密度碳排放中心。③ 黄河流域碳排放呈显著的正的全局空间自相关,并形成了以晋陕蒙资源型城市为依托的中上游碳排放高-高集聚,以及上游甘青宁地区为主的碳排放低-低集聚。④ 经济发展水平对碳排放空间分异的影响力始终最强,其次为城镇化水平与人口规模,“GDP+”能源结构、能源强度与产业结构所主导的交互作用是导致碳排放持续增长的主要推动力。从构建流域生命共同体的视角出发,结合黄河流域自然环境特点与经济社会特征,并统筹上下游、左右岸、干支流之间的关系,分区施策与分时施策并行,对实现以碳减排为目标的黄河流域生态保护与可持续发展意义重大。  相似文献   

Uncertainty of global summer precipitation in the CMIP5 models: a comparison between high-resolution and low-resolution models     

Danqing?HuangEmail author  Peiwen?Yan  Jian?Zhu  Yaocun?Zhang  Xueyuan?Kuang  Jing?Cheng 《Theoretical and Applied Climatology》2018,131(1-2):55-68

Worldwide, the majority of rapidly growing neighborhoods are found in the Global South. They often exhibit different building construction and development patterns than the Global North, and urban climate research in many such neighborhoods has to date been sparse. This study presents local-scale observations of net radiation (Q _* ) and sensible heat flux (Q _H ) from a lightweight low-rise neighborhood in the desert climate of Andacollo, Chile, and compares observations with results from a process-based urban energy-balance model (TUF3D) and a local-scale empirical model (LUMPS) for a 14-day period in autumn 2009. This is a unique neighborhood-climate combination in the urban energy-balance literature, and results show good agreement between observations and models for Q _* and Q _H . The unmeasured latent heat flux (Q _E ) is modeled with an updated version of TUF3D and two versions of LUMPS (a forward and inverse application). Both LUMPS implementations predict slightly higher Q _E than TUF3D, which may indicate a bias in LUMPS parameters towards mid-latitude, non-desert climates. Overall, the energy balance is dominated by sensible and storage heat fluxes with mean daytime Bowen ratios of 2.57 (observed Q _H /LUMPS Q _E )–3.46 (TUF3D). Storage heat flux (ΔQ _S ) is modeled with TUF3D, the empirical objective hysteresis model (OHM), and the inverse LUMPS implementation. Agreement between models is generally good; the OHM-predicted diurnal cycle deviates somewhat relative to the other two models, likely because OHM coefficients are not specified for the roof and wall construction materials found in this neighborhood. New facet-scale and local-scale OHM coefficients are developed based on modeled ΔQ _S and observed Q _* . Coefficients in the empirical models OHM and LUMPS are derived from observations in primarily non-desert climates in European/North American neighborhoods and must be updated as measurements in lightweight low-rise (and other) neighborhoods in various climates become available.  相似文献