陕西镇安县桂林沟钼矿成矿特征及成矿要素分析

潼关—柞水—宁陕区域性北东向构造岩浆岩带控制了矿区岩浆岩体、矿区构造和钼矿化带的产出及其规模,矿区次级断裂构造为成矿物质聚集提供了有利的储存空间,中酸性岩浆活动及其热液蚀变控制了成矿物质的迁移、富集.区域性北东向构造岩浆岩带具有良好的找矿前景,应引起相关矿产勘查工作的高度重视.     

SHRIMP zircon and EPMA monazite dating of granitic rocks from the Maizuru terrane, southwest Japan: Correlation with East Asian Paleozoic terranes and geological implications

Abstract The Maizuru terrane, distributed in the Inner Zone of southwest Japan, is divided into three subzones (Northern, Central and Southern), each with distinct lithological associations. In clear contrast with the Southern zone consisting of the Yakuno ophiolite, the Northern zone is subdivided into the western and eastern bodies by a high-angle fault, recognized mainly by the presence of deformed granitic rocks and pelitic gneiss. This association suggests an affinity with a mature continental block; this is supported by the mode of occurrence, and petrological and isotopic data. Newly obtained sensitive high mass-resolution ion microprobe (SHRIMP) zircon U–Pb ages reveal the intrusion ages of 424 ± 16 and 405 ± 18 Ma (Siluro–Devonian) for the granites from the western body, and 249 ± 10 and 243 ± 19 Ma (Permo–Triassic) for the granodiorites from the eastern body. The granites in the western body also show inherited zircon ages of around 580 and 765 Ma. In addition, electron probe microanalysis (EPMA) monazite U–Th–total Pb dating gives around 475–460 Ma. The age of intrusion, inherited ages, mode of occurrence, and geological setting of the Siluro–Devonian granites of the Northern zone all show similarities with those of the Khanka Massif, southern Primoye, Russia, and the Hikami granitic rocks of the South Kitakami terrane, Northeast Japan. We propose that both the Siluro–Devonian and Permo–Triassic granitic rocks of the Northern zone are likely to have been juxtaposed through the Triassic–Late Jurassic dextral strike-slip movement, and to have originated from the Khanka Massif and the Hida terrane, respectively. This study strongly supports the importance of the strike-slip movement as a mechanism causing the structural rearrangement of the Paleozoic–Mesozoic terranes in the Japanese Islands, as well as in East Asia.     

中日地理学者的论文写作年龄对比分析

以2000年以来的《地理学报》中英文版论文为例,分析了中国地理学者的论文写作年龄特征,包括平均写作年龄、论文写作主体年龄段、高峰期年龄等等,并以日本《地理学评论》为参照,分析了体制环境因素对地理学者论文写作年龄和周期的影响。结果表明,中国地理学母语论文的写作主体是40岁左右年龄段的学者,而英文论文的写作主体是35岁左右年龄段的学者。中国地理学者的母语平均写作年龄要高于日本,但英文论文作者的平均年龄则低于日本,这种差异反映了中日两国在科研管理制度及理念上的不同。在概括分析了两者差异后提出了对中国地理学的学科发展建议。     

三维复杂速度结构中深发地震的双差分定位

双差分地震定位法采用了一维射线追踪法和直角坐标系, 不适合于复杂速度模型中的地震定位.本研究采用三维射线追踪技术和球坐标系改进了双差分定位法, 扩大了它的应用范围.为了检验新方法的可行性和准确性, 以日本海地区下方的深发地震为研究对象, 通过对比4种复杂速度模型中双差分定位结果, 分析速度结构对双差分定位的影响.结果表明, 改进后的双差分定位法受速度结构变化的影响较小, 而且当震源区的速度模型越接近真实速度结构时, 定位结果的精度越高, 这为利用深发地震研究地球深部构造奠定了基础.      

延边东北部地区中生代火山-岩浆岩区金铜矿成矿特征

延边东北部地区中生代陆相火山断陷盆地处于吉黑褶皱系延边优地槽褶皱带延边复向斜内;区内中生代以来不同方向的断裂发育,火山活动强烈,岩浆侵入频繁;与中生代火山-岩浆活动有成因联系的金、铜金金属矿床多处,矿化蚀变线索也较多,构成了著名的五凤-小西南岔近东西向火山-岩浆期后低温热液型金、铜多金属成矿带;区内中生代火山-岩浆岩的形成是太平洋板块俯冲作用使大陆边缘拉张活动不断加剧,造成上地幔岩浆上侵的结果;并伴有成矿作用的发生,在岩浆岩体内外接触带的有利部位形成金、金铜或铜金多金属矿床;从远源至近源的成矿分带为Au-Ag→Au-Cu-Ag→Cu-Au-Pb-Zn→Cu(-Mo-Au);成矿作用表现出从低温至高温、从低硫到高硫的变化.     

改革开放以来东北区城市化与产业结构变动关系研究

总结了改革开放以来东北区城市化发展特点与产业结构变动特点。运用城市化与工业化互动规律、产业结构演变规律和城市化发展规律对东北区城市化与产业结构变动关系进行分析,并探讨了其形成原因。在此基础上,提出了东北区城市化与产业结构协调发展策略:①优化产业结构,加速城市化发展。②以合理的城镇体系结构为载体,促进非农产业的发展。③加强基础设施建设,促进城市化与产业结构的协调发展。     

K–Ar ages of the Akan-Shiretoko volcanic chain lying oblique to the Kurile trench: Implications for tectonic control of volcanism

The Akan‐Shiretoko volcanic chain, situated in the Southwestern Kurile arc, consists mainly of nine subaerial andesitic stratovolcanoes and three calderas. The chain extends in a SW–NE direction for 200 km, situated oblique to the Kurile trench at an angle of 25 degrees. Thirty‐seven new K–Ar ages, plus previous data, suggest that volcanic activity along the Akan‐Shiretoko volcanic chain began at ca 4 Ma at Akan, at the southwestern end of the chain, and systematically progressed northeastward, resulting in the southwest‐northeast‐trending volcanic chain. This spatial and temporal distribution of volcanoes can be explained by anticline development advancing northeastward from the Akan area, accompanied by magma rising through northeast‐trending fractures that developed along the anticlinal axis. The northeastward development of the anticline caused uplifting of the Akan‐Shiretoko area and changed the area from submarine to subaerial conditions. Anticline formation was likely due to deformation of the southwestern Kurile arc, with southwestward migration of the Kurile forearc sliver caused by oblique subduction of the Pacific plate. The echelon topographic arrangement of the Shiretoko, Kunashiri, Etorofu and Urup was formed at ca 1 Ma.     

关于日本渔业调整委员会的性质的探讨

日本的渔业管理有一个显著的特色,就是除了政府相关部门对渔业进行行政管理以外,还有一个特殊的机构－渔业调整委员会参与管理日本沿海各海域的渔业。它既不同于专门的政府机构,又不角我国民间的渔业管理委员会。该机构的建立,使得日本的渔业管理逐步走上了法制化、民主化的轨道。本文通过分析日本渔业法规中对该委员职能的规定,探讨其所具有的性质,期望能为我国今后加强渔业管理提供一定的帮助。     

Genetic types and characteristics of ground ice in Northeast China

１ＧＥＮＥＴＩＣＴＹＰＥＳＯＦＧＲＯＵＮＤＩＣＥＩＮＣＨＩＮＡＧｒｏｕｎｄｉｃｅｉｓｗｅｌｄｅｖｅｌｏｐｅｄｉｎｔｈｅｖｉｃｉｎｉｔｙｏｆｔｈｅｓｏｕｔｈｅｒｎｐｅｒｍａｆｒｏｓｔｌｉｍｉｔｉｎｔｈｅＥｕｒａｓｉａｎｃｏｎｔｉｎｅｎｔ,ｉｎｔｈｅｎ...     

基于重力测点和段差变化的前郭5.8级震群研究与三维反演

利用东北地区近几年流动重力观测数据,分析前郭5.8级震群周边重力点值的时序变化特征,并基于重力段差变化对东北地区整体和局部重力变化引入能够反映异常显著性程度的指标量G和C值,最后对前郭5.8级震群前的重力场动态变化作三维密度反演。结果表明：1）前郭5.8级震群发震构造两侧的局部重力变化具有较明显的差异性,其变化趋势可作为识别构造活化或解耦运动的标志;2）显著性指标量G和C值能够为地震重力前兆的定量描述提供新思路;3）震前重力变化的反演结果显示地震发生在质量运移的过渡区域,垂向反演结果对本次地震的震源深度有一定的揭示意义。