THE ANALYSIS OF TROPICAL CYCLONE PRECIPITATION AFFECTING THE LIAODONG PENINSULA

1 INTRODUCTION Tropical cyclones (TCs) moving north and getting to the Liaodong Peninsula and waters of the Yellow and Bohai Seas are in their late phase of life cycle.While weakening rapidly, TCs carry a large amount of warm and humid air that forms heavy rainfall by itself on the one hand and interact with westerlies in the middle latitudes on the other.     

胶东半岛主要环境工程地质问题及防治对策研究

胶东半岛为我国的工农业生产基地,在沿海经济发展战略中有着重地位。随着地区经济的蓬勃发展和对外开放的不断深入,胶东半岛也面临着日益严峻的环境工程地质问题,对胶东半岛主要环境工程地质问题进行系统研究,并提出综合防治对策与建议。     

Structural study of a semiductile strike-slip system in the Central Iberian Zone (Variscan Fold Belt,Spain): structural controls on gold deposits

The Villalcampo shear system is a regional dextral strike-slip fault zone that affects Late Variscan granites and their metamorphic country rocks over an area of about 150 km². The detailed geometry of this subvertical north-west—south-east shear zone is outlined. The system forms an extensional fan to the northwest and extends to the south-east as a broad extensional duplex. Particular attention is focused on the distribution of fault rocks and associated veins in its north-west splay. A structural study of the shear bands (encompassing both geometric and kinematic criteria) and a microscopic study of the fault rocks has led to the interpretation of the system as a brittle—ductile shear zone. Calculations give a shear strain value of = 1.5 and a minimum displacement of s = 3700 m. The localization of gold mineralization in mylonite-filled subvertical extensional veins is a product of the formation of the Villalcampo shear system. The subvertical faults and veins underwent a process of cyclical sealing and reopening. As such they acted as valves controlled by fluid pressure regulating fluid—rock interactions and gold deposition. Conditions favouring these processes occur near the base of the seismogenic zone in the vicinity of the frictional—quasi-plastic transition at mid-greenschist metamorphic conditions (T = 350°C and 10–15 km depth).     

辽东半岛的环境地质问题与防治对策研究

辽东半岛集中了辽宁省90%的大中型骨干企业、近70%的城市人口和固定资产,创造了辽宁省85%的经济总量,是辽宁省经济发展的龙头地带.本文根据辽东半岛地区地质环境背景条件,研究了不同地区、不同工程活动的环境地质问题,分析了其发育规律与特征,提出了防治环境地质问题的4条举措,即合理开采地下水,可持续利用地区水资源;采取工程...     

雷州半岛海岸带主体功能区划研究

文章采用基于集对分析法的社会、经济与生态环境协调发展模型研究雷州半岛海岸带主体功能区划,确定边界范围,构建评价指标体系。将整个雷州半岛作为海岸带,指标体系划分为三大类共27个指标。赤坎区、坡头区、麻章区属于基本协调发展;开发区（含东海）、遂溪县、雷州市、吴川市、徐闻县和廉江市属于高度协调发展;霞山区属于弱协调或不协调发展。雷州半岛各区域社会、经济发展对环境损害较小。霞山区、开发区（含东海）划分为重点开发区,遂溪县、雷州市、廉江市、吴川市和徐闻县划分为限制开发区,禁止开发区单独划出,包括3个国家级自然保护区、1个国家级风景名胜区和2个国家森林公园。     

Precambrian crustal evolution in Rangrim Massif,Korean Peninsula

Petrological, chronological and geotectonic geological analysis of Precambrian metamorphic rock in Korean Peninsula shows that the remnants （ 〉3.4 Ga） of continental nuclei crust were formed in the Paleoarchean in the Rangrim Massif. In the massif, the main formation ages of continental crust range from 3.2 Ga to 2.5 Ga, its important growing period was 2.8 - 2. 5 Ga. The subsequent expansion period of the Rangrim Massif was 2. 4 - 2. 2 Ga. The division events occurred in 1.85 Ga and in the Late Paleoproterozoic-Early Mesoproterozoic, respectively. Since then the massif was relatively stable. However, the last division of the Rangrim Massif occurred at 793 Ma.     

山东玲珑金矿流体包裹体地球化学特征

玲珑金矿位于胶东半岛招-掖成矿带东部,是我国典型的超大型含金石英脉型金矿。成矿过程可划分为早、中、晚三个阶段,金主要在中阶段沉淀。早阶段流体包裹体为纯 CO_2型(L_(CO_2) V_(CO_2)>90%)和富 CO_2型(10%≤L_(CO_2) V_(CO_2)≤90%),中阶段为纯 CO_2型、富 CO_2型、富 H_2O 型,晚阶段为水溶液包裹体。从早到晚,包裹体均一温度分别集中在240℃～360℃、220℃～360℃、180℃～260℃和80℃～180℃,盐度分别集中在3.4%～10.4%、3.0%～10.2%、4.0%～14.6%和2.4%～5.0%NaCl eqv;早、中阶段流体盐度随温度降低而升高。中阶段第一世代石英中大量水溶液包裹体和富 CO_2包裹体共生,指示流体强烈沸腾。从早到晚,流体包裹体的变化记录了成矿流体性质和构造环境的演化。早阶段石英中沿 X 型节理发育面型包裹体群,既记录了石英脉遭受的剪切变形事件,又记录了同构造流体作用。而充填于张性裂隙的黄铁矿为主的多金属硫化物-石英组合则表明主成矿期构造环境由压性向张性转化,成矿流体系统减压沸腾、逐步开放,并导致金等成矿物质大量沉淀。结合区域构造演化和成矿时间,认为玲珑金矿成矿系统发育在应力场由挤压向伸展转换的构造背景,流体压力变化滞后于构造应力场变化,流体成分以低盐度、富 CO_2为特征,应属典型的造山型金矿系统。     

Potential field constraints on the deep structure of the Lugo gneiss dome (NW Spain)

The Lugo gneiss dome, in the NW Iberian Massif (Spain) is a Variscan structure developed during late stages of orogenic collapse. Crustal extension was mainly accomplished by two kilometre-scale conjugate extensional shear zones and by the late development of the dome and a huge normal fault. These structures overprint previous contractional recumbent folds and a thrust fault. The Lugo dome and its southward continuation, the Sanabria dome, are the site of the conspicuous Eastern Galicia Magnetic Anomaly (EGMA), a N–S band, 50 km wide and 190 km long, with a maximum amplitude of 190 nT. Integrated potential field modelling of the EGMA and its corresponding gravity signature have been carried out aided by constraints provided by the measurement of c. 900 magnetic susceptibilities and by previous geophysical data, mainly seismic refraction and reflection profiles. Results suggest that a large volume of low-density migmatites and associated inhomogeneous granites are the main source of the magnetic anomaly. Small massifs of basic and ultrabasic rocks inside the migmatites and high-susceptibility iron ore bodies sparsely distributed in low-grade Middle Ordovician slates are also thought to contribute to the anomaly but to a minor extent. Although otherwise similar to other gneiss domes, the Lugo dome is accompanied by a striking magnetic anomaly whose origin is discussed in terms of the tectonic evolution of this structure and the provenance of the magnetite-bearing migmatites and inhomogeneous granites that core it.