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61.
Journal of Oceanology and Limnology - Although the impact of ocean acidification on marine bivalves has been previously investigated under mainly controlled laboratory conditions, it is still... 相似文献
62.
西藏拉萨地体榴辉岩的地球化学特征和Sm-Nd、Rb-Sr同位素组成及其地质意义 总被引:2,自引:0,他引:2
最近在青藏高原拉萨地体新发现了一条榴辉岩带,该榴辉岩带位于冈底斯岩浆岛弧带的北缘。对该带榴辉岩的岩石地球化学特征及SmNd、RbSr同位素组成研究表明: ① 该带榴辉岩的原岩主要是一套低钾的大洋拉斑系列玄武岩,其原岩类似于典型的NMORB,源于亏损地幔; ② 该带榴辉岩样品 (87Sr/86Sr)i=0.70335~0.70457,变化范围较大,且与εNd(t)值及微量元素特征均没有好的对应关系,可能是由于该套岩石形成于大洋环境,形成后遭受了海水的蚀变作用;(3)该带榴辉岩全岩的SmNd等时线年龄为305.5±50Ma (2σ),(143Nd/144Nd)i=0.5126±0.00007 (2σ),表明该带榴辉岩可能形成于早石炭-晚二叠世,在这一时期冈底斯北缘可能存在古特提斯洋盆及古特提斯洋盆深俯冲作用。 相似文献
63.
Carbonate minerals and water (or geofluids) reactions are important for modeling of geochemical processes and have received considerable attention over the past decades.The calcite dissolution rates from 50℃to 250℃at 10 MPa in deionized water with a flow rate varying from 0.2 to 5 mL/min were experimentally measured in a continuous flow column pressure vessel reactor.The dissolution began near the equilibrium with c/c_(eq)>0.3 and finally reached the equilibrium at 100℃-250℃,so the corresponding solubility was also determined as 1.87,2.02,2.02 and 1.88×10~(-4)·mol/L at 100℃,150℃,200℃and 250℃respectively,which was first increasing and then switching to decreasing with temperature and the maximum value might occur between 150℃and 200℃.The experimental dissolution rate not only increased with temperature,but also had a rapid increase between 150℃and 200℃at a constant flow rate of 4 mL/min.The measured dissolution rates can be described using rate equations of R=k(1-c/c_(eq))n or R=kc~(-n).In these equations the reaction order n changed with temperature,which indicates that n was a variable rather than a constant,and the activation energy was 13.4 kJ/mol calculated with R=k(1-c/c_(eq))~n or 18.0 k J/mol with R=kc~(-n),which is a little lower than the surface controlled values.The varied reaction order and lower activation energy indicates that calcite dissolution in this study is a complex interplay of diffusion controlled and surface controlled processes. 相似文献
64.
The Structure of Ore-controlling Strain and Stress Fields in the Shangzhuang Gold Deposit in Shandong Province, China 总被引:22,自引:0,他引:22
DENG Jun WANG Qingfei YANG Liqiang ZHOU Lei GONG Qingjie YUAN Wanming XU Hao GUO Chunying LIU Xiangwei 《《地质学报》英文版》2008,82(4):769-780
The Shangzhuang altered-rock type gold ore deposit is located in the middle segment of and controlled by the Wang'ershan fault zone in the northwestern part of the Jiaodong gold province, China. The deformation evolution, the structure of strain and stress fields and its ore-controlling effect in the Shangzhuang deposit are discussed in this paper. It is revealed that the deformation evolution has mainly undergone four phases: the early ductile deformation, the second NE-striking horizontal simple shear, the third NE-striking compression-shear and the final NW-striking compression. The mineralization happened during the third stage in which the maximum principal stress gradually transited from NE to NW. The 3-D numerical simulations of the stress field show that, on the condition that the maximum principal stress is NE-striking, the fracture development in the fault zone is favored, while when the maximum principal stress is NW-striking, the fault zone is relatively extensional and it is suitable for the influx and emplacement of ore-forming fluids. The compression-shear strain field during the mineralization is characterized by the λ-type structure, the positive flower structure, etc. Orebodies are mostly equidistantly located in the dilatational spaces, which are distributed in the integral compressional circumstances. And the dilatational spaces are developed where the fault attitude changes or shear joint systems develop. In the overall compression-shear stress field, the strain field bears self-similarity at multiple scales, including the orebody, ore deposit and orefield. The selfsimilarity of the structure comprises the subequidistant distribution of fractures at the same scale and the similar shape of the fractures at various scales. Yet, due to the special geological structure, the orebodies are mostly located in the hanging wall in the Shangzhuang deposit, which is different from most deposits in the Jiaodong gold province. Analyses of the ore-controlling stress and strain fields in the deposit pro 相似文献
65.
对几种不同结构的岩石标本在变形过程中声发射b值和频谱随时间的变化特征进行了对比研究 ,其中包括完整花岗岩标本、含有天然愈合节理的花岗岩标本、含有拉张型和挤压型雁列式断层以及平直断层的标本等。研究表明 ,声发射b值和频谱的特征不仅会受标本结构的影响 ,而且在同一标本的不同变形阶段也可能表现出不同的特征 ,其机制与变形方式以破裂为主或以摩擦为主有关。当变形以破裂为主时 ,声发射b值和频谱在失稳前会出现明显的下降 ;当变形以摩擦为主时 ,声发射b值和频谱在失稳前变化相对较小 ,且上升或下降均可能出现。实验结果意味着b值和频谱特征作为失稳前兆 ,在不同的构造环境下可能会有不同的特征 ,而强震孕震区内不同断裂构造的存在会造成前兆时空分布的非均匀性 相似文献
66.
The Influence of Undersea Feature Naming on Delimitation of Continental Shelf: A Case Study of Japan
Base on the tracing study on the Japanese undersea feature naming activity, this study shows that, Japan has named Bando Basin, removed Hangetsu Trough, Shingetsu Hole and Oki-Daito Trough, and altered some features names near Ogasawara Plateau and Oki-Daito Ridge, before and after the submission for Delimitation in outer limits of continental shelves. Contrary to the general undersea feature naming rule, these actions aim to extend its continental shelf boundaries. It is suggested that the study of relationships between naming undersea feature and marine right and interest should be enhanced. 相似文献
67.
Liqiang Zhang Zhizhong Kang Jonathan Li Ling Yang 《International Journal of Applied Earth Observation and Geoinformation》2010
This paper presents a Web-based three-dimensional Geographic Information System (3DGIS) for Wenchuan earthquake disaster assessment. With the help of information technology resources, geoscientists are in a position to learn more about the structure of the earthquake in efficient ways. Due to huge spatial datasets of Wenchuan, China and narrow network bandwidth, general-purpose applications are difficult to transmit and visualize these datasets on the network. The application aims to interactively represent and transfer large spatial objects of Wenchuan County, China, as well as for dynamically rendering them in networking environments. Level-of-detail (LOD) terrain models and vector maps are created, and the server–client architecture is presented. The application provides an effective way for powerful access and manipulation of large-scale Wenchuan datasets. 相似文献
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70.
多普勒雷达资料在冷涡强对流天气中的同化应用试验 总被引:3,自引:0,他引:3
应用WRF模式的三维变分同化系统(WRF-3DVAR),对沈阳多普勒天气雷达资料在东北冷涡暴雨个例中的同化应用进行了试验.研制了多普勒雷达资料质量控制系统,实现了对径向风和反射率因子的直接同化,不但可以反演中尺度三维气象要素场,而且可以为模式提供初始场.以天气尺度资料为背景场同化多普勒雷达资料,WRF-3DVAR可以较好地反演冷涡中尺度对流系统的三维结构,反演的地面强对流辐散气流及在对流层中层涡旋都符合中尺度系统概念模型,通过与实际地面探测资料进行了对比,风场环流基本接近,同化了雷达资料的气象要素场可为预报业务提供较好的包含中小尺度系统的实时三维分析场.通过冷涡个例同化试验,应用WRF-3DVAR同化雷达资料后,中尺度模式对对流降水的预报总体有正的影响,对强对流中的一些中小尺度雨团的预报也略有改善. 相似文献