Earthquake Monitoring and Study in the Jingpohu Volcano Cluster Area

Seismicity in the Jingpohu volcanic area was investigated based on the seismic data recorded by the mobile seismic network consisting of 14 stations equipped with 24-bit broad-band 3- component seismographs around Crater Forest, Results show that there appears certain seismicity in Jingpohu and its adjacent areas with a low activity level and most of the recorded earthquakes are the volcanic-tectonic ones, The results of location indicate a dominant focal depth of 10km - 30kin, most of the earthquakes are smaller than ML2,0, and are concentrated in the area of ＂ Crater Forest＂ and on the Dunhua-Mishan fault which runs through the volcanic area. At station No. 2, which has better observation conditions, two types of events, likely associated to volcanism, were recorded; their waveform characteristics are somewhat similar to that of the long-period volcanic event and the volcanic tremor, but with different feature of frequencies.     

The distribution rule and seepage effect of the fractures in the ultra-low permeability sandstone reservoir in east Gansu Province,Ordos Basin

To study the impact of the fractures on development in the ultra-low permeability sandstone reservoir of the Yangchang Formation of the Upper Triassic in the Ordos Basin,data on outcrops,cores,slices,well logging and experiments are utilized to analyze the cause of the formation of the fractures,their distribution rules and the control factors and discuss the seepage flow effect of the fractures. In the studied area developed chiefly high-angle tectonic fractures and horizontal bedding fractures,inter-granular fractures and grain boundary fractures as well. Grain boundary fractures and intragranular fractures serve as vital channels linking intragranular pores and intergranular solution pores in the reservoir matrix,thus providing a good connectivity between the pores in the ultra-low perme-ability sandstone reservoir. The formation of fractures and their distribution are influenced by such external and internal factors as the palaeo-tectonic stress field,the reservoir lithological character,the thickness of the rock layer and the anisotropy of a layer. The present-day stress field influences the preservative state of fractures and their seepage flow effect. Under the tec-tonic effect of both the Yanshan and Himalayan periods,in this region four sets of fractures are distributed,respectively assuming the NE-SW,NW-SE,nearly E-W and nearly S-N orientations,but,due to the effect of the rock anisotropy of the rock formation,in some part of it two groups of nearly orthogonal fractures are chiefly distributed. Under the effect of the present-day stress field,the fractures that assume the NE-SW direction have a good connectivity,big apertures,a high permeability and a minimum starting pressure,all of which are main advantages of the seepage fractures in this region. With the development of oilfields,the permeability of the fractures of dif-ferent directions will have a dynamic change.     

Petrology of the Yugu peridotites in the Gyeonggi Massif,South Korea: Implications for its origin and hydration process

Peridotites exposed in the Yugu area in the Gyeonggi Massif, South Korea, near the boundary with the Okcheon Belt, exhibit mylonitic to strongly porphyroclastic textures, and are mostly spinel lherzolites. Subordinate dunites, harzburgites, and websterites are associated with the lherzolites. Amphiboles, often zoned from hornblende in the core to tremolite in the rim, are found only as neoblasts. Porphyroclasts have recorded equilibrium temperatures of about 1000°C, whereas neoblasts denote lower temperatures, about 800°C. Olivines are Fo_90–91 in lherzolites and Fo₉₁ in a dunite and a harzburgite. The Cr# (= Cr/(Cr + Al) atomic ratio) of spinels varies together with the Fo of olivines, being from 0.1 to 0.3 in lherzolites and around 0.5 in the dunite and harzburgite. The Na₂O content of clinopyroxene porphyroclasts is relatively low, around 0.3 to 0.5 wt% in the most fertile lherzolite. The Yugu peridotites are similar in porphyroclast mineral chemistry not to continental spinel peridotites but to sub‐arc or abyssal peridotites. Textural and mineralogical characteristics indicate the successive cooling with hydration from the upper mantle to crustal conditions for the Yugu peridotites. Almost all clinopyroxenes and amphiboles show the same U‐shaped rare earth element (REE) patterns although the level is up to ten times higher for the latter. The hydration was associated with enrichment in light REE, resulting from either a slab‐derived fluid or a fluid circulating in the crust. The mantle‐wedge or abyssal peridotites were emplaced into the continental crust as the Yugu peridotite body during collision of continents to form a high‐pressure metamorphic belt in the Gyeonggi Massif. The peridotites from the Gyeonggi Massif exhibit lower‐pressure equilibration than peridotites, with or without garnets, from the Dabie–Sulu Collision Belt, China, which is possibly a westward extension of the Gyeonggi Massif.     

土钉支护结构破坏模式和加固机制分析

对不同土质中土性参数和支护参数共同影响下基坑土钉支护结构的内力和位移进行了系统的数值试验研究。结果表明,从砂土到粉土,再到软黏土介质变化时,基坑位移大小剧增,位移形态也发展成下部凸出的流鼓状,而且中下部土钉不能满足承载力要求。土性参数中,内摩擦角和凝聚力是导致位移形态发生改变的主要因素,侧压力系数主要引起位移大小的变化。支护参数中,土钉密度突出控制钉间土体位移;土钉长度在砂土中控制上部位移显著,软黏土中抑制下部位移更明显;土钉刚度的影响体现为钉土刚度比的影响,主要由插筋刚度控制,而随土类变化并不明显;并得出了各支护参数的临界值。     

两淮地区煤炭资源地质勘探类型定量综合评价方法

安全、高效的现代化矿井建设,要求煤炭资源勘探速度快、精度高。通过总结安徽两淮地区近几十年来煤炭资源综合勘探经验,围绕“高精度、快速勘探”的主题,采用恰当的评价指标,对煤层稳定性和构造复杂程度进行定量评价,并提出了本地区煤炭资源地质勘探类型定量综合评价原则和方法,开发了定量评价软件系统。实际应用效果证明,该方法可行,结果可靠。      

几种海洋蓝藻生长条件的研究

对Ｓｙｎｅｃｈｏｃｏｃｃｕｓ ｂａｃｉｌｌａｒｉｓ，Ｏｓｃｉｌｌａｔｏｒｉａ ｌｕｄ，Ｓｃｈｉｚｏｔｈｒｉｘ ｃａｌｃｉｃｏｌａ，Ｓｐｉｒｕｌｉｎａ ｐｌａｔｅｎｓｉｓ等４各海洋蓝藻的生长条件的研究表明，除Ｓ．ｐｌａｔｅｎｓｉｓ外，其他３种蓝藻在“ｆ／２”培养基中生长良好，外源生长因子对生长有不同程度的促进作用。Ｓ．ｂａｃｉｌｌａｒｉｓ适应较高光强，其温度和ｐＨ最适范围较窄，Ｓ．ｃａｌｃｉｃｏｌａ     

省域发展潜力影响要素及其作用机理分析

围绕区域发展潜力来源,建构了区域发展潜力影响要素分析框架,论述了外部环境、内部资源、内部能力的组成及其影响机理。得出：区域发展阶段不同,区域发展潜力影响因素的类型与质量存在分异。且不同发展阶段下发展潜力主导影响因素呈现：（1）处于农业经济主导和工业化初期的区域,受控于自然资源与条件、人口与劳动力;（2）处在工业化中、末期的区域,主导因素是区域经济基础、人力资本和发展战略;（3）处在后工业化和信息时代的区域,区域能力是其主导因素。     

数字地名词典中的类型表达和管理

在数字地名词典中恰当地表达和管理地名的类型知识,有助于数字地名词典快速、有效地处理地名相关查询.为此,该文首先从数字地名词典的应用需求出发,分析类型在数字地名词典中的作用,进而设计一个地名类型本体模型.该模型表达了地名类型之间的继承关系以及对空间关系的约束.在本体模型基础上,提出了相应的查询处理策略并进行了系统实现.     

新疆旅游资源的类型、等级及空间分布特征

在全面掌握新疆旅游资源的实查资料基础上,对全疆旅游资源做系统分类与定量评价,总结其类型、等级和空间分布特征,并从新疆地理环境变迁和多民族、多文化的社会环境两方面分析新疆高品质旅游资源的成因。结果表明:新疆旅游资源类型多样,与全国相比,主类、亚类齐全,基本类型占66.5%;八大类中建筑与设施和地文景观的种类较丰富;建筑与设施类景点最多,水域风光和生物景观次之;新疆旅游资源等级较高,优良级占43.6%,整体为中间大两头小的谷仓型结构;高等级集中于凸峰、观光游憩湖区、林地、草地、野生动物栖息地、废城与聚落地、石窟、边境口岸、特色街巷、传统手工产品与制品、民间演艺等类;空间分布呈现为三带两环状和六点状集聚特征,这与新疆地貌格局和高品质景点的聚群作用有关;新疆自然旅游资源是整个地理环境演变过程的产物;而多民族、多文化的社会环境是人文类的主要成因。