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991.
广州市商业型健身房空间分布及其影响因素 总被引:1,自引:0,他引:1
以百度地图网页上采集的POI数据和第六次人口普查数据为基础,借助ArcGIS 10.2和Geoda软件,通过核密度分析、方向分布分析、缓冲区分析、近邻分析和空间自相关等方法,对广州市商业型健身房的空间分布特征进行研究,结果表明:广州市商业型健身房在空间分布上呈现“中心圈层+外围组团”结构,存在空间集聚现象以及沿城市干道和地铁站分布指向性不明显而呈现临近住宅小区分布指向性。在广州市商业型健身房空间分布的影响因素方面,经过模型比较,选择空间滞后模型对其进行定量分析,结果表明:人口规模与受教育水平对广州市商业型健身房的空间布局影响显著,而区位因素和社区环境影响力较小。 相似文献
992.
993.
南京汤山洞穴石笋稳定同位素指示的气候与环境意义 总被引:15,自引:1,他引:15
对南京汤山葫芦洞南壁钙板上一支长82mm石笋进行了高精度热电离质谱(TIMS)定年及氧碳同位素分析。结果表明,该支短石笋生长时段长达300ka左或(距今463~159ka),其底部年龄进一步证实南京直立人生存时代早于450kaBP。δ^13C值在MIS6/7界线上的显著漂移揭示了一次土壤侵蚀事件,结束了洞穴文化层的堆积历史。 相似文献
994.
青藏高原腹地湖泊沉积序列与古气候变化 总被引:12,自引:4,他引:12
在青藏高原综合科学考察中,选择其腹地系列剖面的沉积物记录进行地层气候学和同位素气候学的研究。沉积物记录的气候变化与同位素丰度变化的响应关系十分吻合,其时间尺度和分辨率也能够互为补偿,在较大范围内覆盖了32kaBP以来的古气候环境变化。更为有意义的是,清晰准确地检出新仙女木期气候冷干颤动事件,用同位素丰度变化拟合的降温幅度可达11C;并且识别出“仙女木期”(包括老-中-新仙女木事件)高分辩率气候变化 相似文献
995.
从波动观点看塔北地区油气藏的形成演化:以英买7油藏为例 总被引:6,自引:0,他引:6
本文运用沉积波动过程分析方法,在综合分析野外露头、岩心、录井、测井、地震等资料的基础上,建立了塔北地区不同小区的岩性-时间剖面。研究表明,740 ̄760Ma、200 ̄240Ma、100 ̄110Ma、60 ̄70Ma、30Ma是控制塔北地区构造演化的主要周期。早古生代、三叠纪和第三纪以来是3次主要的沉积高峰,志留纪末-晚泥盆世早期为主要肃蚀期,肃蚀量一般〉1000m,北部〉1500 ̄2000m,海西期 相似文献
996.
Continental- Margin Structure of Northeast China and Its Adjacent Areas 总被引:10,自引:0,他引:10
Tang Kedong Shenyang Institute of Geology Mineral Resources Shenyang Liaoning ProvinceWang Ying Bureau of Geology Mineral Resources of Heilongjiang Province Harbin HeilingjiangHe Guoqi Shao Ji''an Peking U niversity Beijing Liu Xinzhu 《《地质学报》英文版》1995,69(3):241-258
The continental margin of Northeast China and its adjacent areas is composed of two tectonic belts. The inner belt is a collage made up of fragments resulting from breakup of an old land with the north part related to the evolution of the Palaeo-Asian Ocean and the south part to the evolution of the Palaeo - Pacific Ocean. The outer belt is a Mesozoic terrane, which is a melange made up of fragments of the Late Palaeozoic to Early Mesozoic oceanic crust and the Late M esozoic trench accumulations.There existed another ocean-the Palaeo - Pacific Ocean during the period from the closing of the Palaeo-Asian Ocean to the opening of the modern Pacific Ocean or from the Devonian to Jurassic, and the ocean-floor spreading of the Palaeo - Pacific Ocean led to the formation of the above-mentioned tectonic belts. The development of the strike-slip fault system after the Late Jurassic and the formation of an epicontinental volcano -plutonic rock belt in the Late Cretaceous to Early Tertiary are attributed to the i 相似文献
997.
Structural Evidence for the in-situ Origin of the HP and UHP Eclogites in the Dabie-Sulu Orogenic Belt 总被引:3,自引:1,他引:3
ZHONG Zengqiu YANG Qijun SUO Shutian ZHOU Hanwen YOU Zhendong China University of Geosciences Wuhan Hubei E-mail: zqzhong@cug.edu.cn Hao Ziguo Liu Xinzhu 《《地质学报》英文版》2003,77(3):304-310
Whether the HP and UHP metamorphic rocks of the Dabie-Sulu orogenic belt are of an "in-situ" or "foreign" origin is a long-standing dispute among geologists. Eclogites preserved today in the HP and UHP units constitute merely 5-10%, which are not isolated exotic bodies tectonically intruding into amphibolite facies gneiss, but remnants of once pervasive or widespread eclogite-facies terranes or slabs. The present spatial distribution and forms of the eclogites have resulted from polyphase and progressive deformation and strain partitioning of the HP and UHP slabs. From their formation in deep mantle to their exhumation to the surface, the eclogites have experienced long-term deformation with different strain regimes. The dominant regime responsible for the present spatial distribution and forms of the eclogites is the shear process. The deformation patterns of the eclogites and gneiss matrix also clearly show that the eclogites were metamorphosed in situ. The original distribution area of the eclogites 相似文献
998.
LIU Shen HU Ruizhong FENG Caixi CHI Xiaoguo LI Cai YANG Rihong WANG Tianwu JIN WeiGuiyang Institute of Geochemistry Chinese Academy of Sciences Guiyang Guizhou E-mail: lliushen@hotmail.comGraduate School of the Chinese Academy of Sciences Beijing College of Earth Sciences Jilin University Changchun Jilin Aero Geophysical & Remote Sensing Center Beijing 《《地质学报》英文版》2003,77(2):187-193
Volcanic rocks in the study area, including dacite, trachyandesite and mugearite, belong to the intermediate-acid, high-K calc-alkaline series, and possess the characteristics of adakite. The geochemistry of the rocks shows that the rocks are characterized by SiO2>59%, enrichment in A12O3(15.09-15.64%) and Na2O (>3.6%), high Sr (649-885 μg/g) and Sc, low Y contents (<17 μg/g), depletion in HREE (Yb<1.22 μg/g), (La/Yb)N>25, Sr/Y>40, MgO<3% (Mg<0.35), weak Eu anomaly (Eu/Eu=0.84-0.94), and lack of the high field strength elements (HFSE) (Nb, Ta, Ti, etc.). The Nd and Sr isotope data (87Sr/86Sr=0.7062-0.7079, 143Nd/144Nd=0.51166-0.51253, εNd= -18.61-0.02), show that the magma resulted from partial melting (10%-40%) of newly underplated basaltic lower crust under high pressure (1-4 GPa), and the petrogenesis is obviously affected by the crust's assimilation and fractional crystallization (AFC). This research will give an insight into the uplift mechanism of the Tibetan plateau. 相似文献
999.
HAO Weicheng SUN Yuanlin JIANG Dayong YANG Shouren WANG Xinping Geological Museum Peking University Beijing 《《地质学报》英文版》2003,77(4)
The "Falang Formation" of western Guizhou was previously called the "Halobia Bed" and considered to be I .adinian in age. It was subdivided upward into the Zhuganpo, Laishike and Longchang members based on ammonites and the Trachyceras multitubertulatum Zone of the Longchang Member was put in the Lower Carnian. Here in the present paper, 4 genera and 9 species of ammonites and 1 nautiloid genus and species collected from the upper part of the "Falang Formation" (i.e. the Wayao Formation used in this paper, equivalent to the Laishike Member from Guanling and Zhenfeng counties are described. The geological and geographical distribution of these cephalopods, as well as the co-existing conodonts, put the Wayao Formation to the late early Carnmian. 相似文献
1000.
The Sequence of Magmatic-Tectonic Events and Orogenic Processes of the Yanshan Belt, North China 总被引:11,自引:0,他引:11
DENG Jinfu SU Shangguo MO Xuanxue ZHAO Guochun XIAO Qinghiu JI Guangyi QIU Ruizhao ZHAO Hailing LUO Zhaohu WANG Yang LIU Cui China University of Geosciences Beijing and Key Laboratory of Lithospheric Tectonics Lithoprobe Techniques Ministry of Education of China 《《地质学报》英文版》2004,78(1):260-266
This paper emphasizes that the interactive constraints of geology and isotopic dating is the best approach to construct the geological event sequence, and has compiled 106 data of reasonable isotopic ages for the igneous rocks of the Yanshan belt. We propose a sequence of mgmatic-tectonic events in the Jurassic-Cretaceous Yanshan orogen of North China. Five orogenic episodes are divided, (1) pre-and initial orogenic episode (Early Jurassic); (2) early orogenic episode (Middle Jurassic); (3) peak orogenic episode (Late Jurassic); (4) late orogenic episode (early Early Cretaceous), and (5) post-orogenic episode. Each episode is a short cycle, all of the orogenic processes construct a longer cycle, and they, in general, followed a counter-clockwise (ccw) PTt path. Finally, it is suggested that the Yanshanian movement was so intensive that the magmatism and tectonic deformation had involved all the lithosphere thickness and the late-Achaean-formed cratonic lithosphere had been significantly reworked. 相似文献