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121.
将中国沿海省区17个中心城市服务业水平分为全面发展型、发达型、次发达型和欠发达型。通过服务业以及服务业与城市之间的关系分析得出:发达型、次发达型服务业的人均服务产品占有量与增加值比重以及就业比重均呈正相关关系,且相关性随着服务业绝对水平的提高而增强;欠发达型服务业的人均服务产品占有量与增加值比重以及就业比重均呈负相关的关系;任何水平类型的服务业的增加值比重与就业比重之间都为正相关。服务业绝对水平与城市人均GDP、城市综合竞争力、城市规模之间都呈正相关;比重规模与城市经济水平之间无明显相关性。 相似文献
122.
We infer the groundwater-level anomalies associated with a hypothetical preslip prior to the anticipated M 8 Tokai earthquake,
and evaluate the detectability of the anomalies using data from seven groundwater wells. We evaluate the detectability of
the anomalies under the following assumptions: (1) an Mw 5.5–6.5 aseismic preslip event occurs at the plate boundary in and
around the hypothetical focal zone of the Tokai earthquake; (2) the total amount of the strain step at each observation associated
with the preslip can be calculated by tensile and shear faulting based on the dislocation model; (3) a normalized strain history
associated with the preslip is defined from the results of numerical simulations based on rate- and state-dependent friction
laws; and (4) the groundwater-level anomaly prior to the earthquake is proportional to the estimated history of the strain
change associated with the preslip. We investigate the detection time of the anomaly at seven wells given an Mw 5.5, 6.0,
or 6.5 aseismic preslip at one of the 272 grid points in and around the area of the hypothetical focal zone of the Tokai earthquake.
As a result, over the time interval between 1 and 48 hours prior to the hypothetical Tokai earthquake, we are able to detect
at each of the seven wells a hypothetical Mw 6.5 preslip at 10–86 of the 272 grid points, an Mw 6 preslip at 0–19 grid points,
and an Mw 5.5 preslip at 0–5 grid points. 相似文献
123.
TSAI Chinglang WEI Kunghua WANG Chenshu Department of Earth Sciences National Cheng Kung University Tainan Taiwan China 《《地质学报》英文版》2002,76(1):31-43
The basement of the central Qilian fold belt exposed along the Minhe-Ledu highway consists of psammitic schists, metabasitic rocks, and crystalline limestone. Migmatitic rocks occur sporadically among psammitic schist and metabasitic rocks. The mineral assemblage of psammitic schist is muscovite + biotite + feldspar + quartz ± tourmaline ± titanite ± sillimanite and that of metabasitic rocks is amphibole + plagioclase + biotite ± apatite ± magnetite ± pyroxene ± garnet ± quartz. The migmatitic rock consists of leucosome and restite of various volume proportions; the former consists of muscovite + alkaline feldspar + quartz ± garnet ± plagioclase while the latter is either fragments of psammitic schist or those of metabasitic rock. The crystalline limestone consists of calcite that has been partly replaced by olivine. The olivine was subsequently altered to serpentine. Weak deformations as indicated by cleavages and fractures were imposed prominently on the psammitic schists, occasionally on me 相似文献
124.
DONG Shuwen Chinese Academy of Geological Sciences Baiwanzhuang Ro Beijing WU Hongling LIU Xiaochun XUE Huaimin Institute of Geomechanics Chinese Academy of Geological Sciences Beijing Fei Zhenbi 《《地质学报》英文版》2002,76(1):69-80
Up to now it is known that almost all ultrahigh-pressure (UHP) metamorphism of non-impact origin occurred in continent-continent collisional orogenic belt, as has been evidenced by many outcrops in the eastern hemisphere. UHP metamorphic rocks are represented by coesite- and diamond-bearing eclogites and eclogite facies metamorphic rocks formed at 650-800℃ and 2.6-3.5 GPa, and most of the protoliths of UHP rocks are volcanic-sedimentary sequences of continental crust. From these it may be deduced that deep subduction of continental crust may have occurred. However, UHP rocks are exposed on the surface or occur near the surface now, which implies that they have been exhumed from great depths. The mechanism of deep subduction of continental crust and subsequent exhumation has been a hot topic of the research on continental dynamics, but there are divergent views. The focus of the dispute is how deep continental crust is subducted so that UHP rocks can be formed and what mechanism causes it to be subducte 相似文献
125.
羌塘中部雀莫正长斑岩体特征及构造意义 总被引:2,自引:0,他引:2
雀莫正长斑央全碱含量较高且K2O>Na2O,富集大离子亲石元素,轻重稀土元素比值较高,稀土元素配分曲线呈斜率较大的右倾式,副矿物组合为磷灰石-榍石-磁铁矿,时代属喜马拉雅期,构造上属造山晚期侵入体。 相似文献
126.
该文阐述了透视坐标系的概念 ,列举了多种透视坐标网中量化信息的图解实例 ,力求进一步丰富和提高专题地图图形可视化的表现能力。 相似文献
127.
128.
129.
西藏羌塘中央隆起区物质组成与构造演化 总被引:7,自引:0,他引:7
对羌塘中央隆起区的物质成分及构造演化规律的认识 ,涉及到青藏高原特提斯演化、羌塘盆地的形成发展及高原的隆升过程。对羌塘中央隆起区构造演化在认识上目前有较大分歧 ,主要有两种观点 :1)认为扎布 (察布 )—查桑地区发育裂谷 ,没有发育成特提斯洋盆 ;2 )龙木错—双湖 (—澜沧江 )古特提斯缝合带 ,代表古特提斯洋的闭合遗迹之一。基于对羌塘中央隆起区物质成分及属性 ,以及同位素年代学研究 ,将羌塘中央隆起中泥盆世—早白垩世的构造发展历史划分了六个阶段 ,即D2 —C11初始裂谷阶段 ;C21—C2 裂谷阶段 ;P1海底扩张—大洋化阶段 ;P2 —T2 板块汇聚—消减阶段 ;T3 —J1板块碰撞阶段 ;J2 —K1碰撞—整体抬升阶段。羌塘中央隆起构造演化经历了一个完整的威尔逊旋回 相似文献
130.
中太平洋海山多金属结壳的成矿特征 总被引:10,自引:0,他引:10
根据我国大洋多金属结壳的调查资料并结合其他相关的研究结果,对中太平洋海山区多金属结壳的类型,产状,成分,结构,分布等成矿特征进行了初步的研究,结果表明,中太平洋海山区富钴结壳广泛发育,但成矿特征较大地受地形,水溶,基岩类型等成矿环境因素的影响与制约。 相似文献