震旦纪地层黄铁矿硫同位素组成时－空变化特征及扬子地块与晚元古超大陆关系的论证

扬子地区早震旦世时期沉积岩黄铁矿具有重的硫同位素组成,其δ¹⁴S值从早震旦世椿木组地层的24‰左右逐渐变得更正。在早震旦世扬子地区广泛沉积碳酸锰矿和黑色页岩的民乐组时期达到极正值+60‰,然后又降低至+16‰-+20‰。上述硫同位素组成的时-空变化特征支持了扬子地块属晚元古Rodinia超大陆的一个组成部分的假设。从晚震旦世早期陡山沱组底部开始,沉积岩中黄铁矿硫同位素的δ¹⁴SS出现负值,并继续降低至-27‰以下。早震旦世晚期-晚震旦世早期沉积岩中硫同位素组成特征反映了沉积盆地古海洋环境的剧烈变化,它与大约7亿年时Rodinia超大陆的解体以及扬子地块与其它大陆分离的地质推测相吻合。     

Contrasting provenance of Late Archean metasedimentary rocks from the Wutai Complex, North China Craton: detrital zircon U–Pb, whole-rock Sm–Nd isotopic, and geochemical data

Detrital zircon U–Pb ages, whole-rock Nd isotopic, and geochemical data of metasedimentary rocks from the Wutai Complex in the Central Zone, North China Craton, have been determined. Compositionally, these rocks are characterized by a narrow variation in SiO₂/Al₂O₃ (2.78–3.96, except sample 2007-1), variable Eu anomalies, spanning a range from significantly negative Eu anomalies to slightly positive anomalies (Eu/Eu* = 0.58–1.12), and positive ε _Nd (t) values (0.1–1.97). The 18 detrital zircons of one sample yielded age populations of 2.53 Ga, 2.60 Ga, and 2.70–2.85 Ga. Geochemical data reveal intermediate source weathering, varying degrees of K-metasomatism in the majority of these metasedimentary rocks, whereas other secondary disturbances seem to be negligible. Detailed analysis in detrital zircon U–Pb geochronology, whole-rock Nd isotope, and geochemistry shows that these metasedimentary rocks are derived from a mixed provenance. The predominant derivation is from the late Archean granitoids and metamorphic volcanics in the Wutai Complex, and there is also input of older continental remnants, except TTG gneisses, from the Hengshan and Fuping Complexes. The sediments were probably deposited in fore-arc or/and intra-arc basins within an arc system.     

基于电磁驱动的滑坡模型水分迁移理论及试验研究

加快模型试验中水的渗流速率对库岸滑坡研究意义重大。考虑滑坡渗流特性,基于电磁驱动原理,在滑坡模型中施加相互垂直的电场、磁场,推导出孔隙水受力公式,根据电渗固结理论,推导水分迁移速率v与电压Ve、磁场强度B的关系式,进而获得时间相似比,实现了通过电磁场强度来控制滑坡模型水分迁移速率,改进模型试验,为研究库水位升降对滑坡的影响提供条件。通过试验进行验证：电磁场对水分迁移速度的影响具有显著效果,且电压大小对模型的稳定渗流场影响较小。说明在不改变模型材料参数的条件下,改变磁场强度和电压可获得任意孔隙水的渗流速度,为研究库水位波动条件下的滑坡演化机制奠定基础。     

A new quasar identified in the vicinity of NGC1068

An X-ray source close to the classical Seyfert galaxy NGC 1068 is identified as a quasar with a redshift of 0.63. The very high surface density of quasars around NGC 1068 suggests that the quasars may be physically associated with this active galaxy.     

Damage of 1975 Haicheng Ms7.3 earthquake in the Korean Peninsula and its effect on Kyushu, Japan

The 1975 Haicheng MS7.3 earthquake affected whole Korean Peninsula and even Kyushu,Japan.In this paperisoseismal map of this earthquake was drawn for these areas by sorting out and analyzing data systematically col-lected,furthermore,the characteristics of the earthquake damage were discussed.In the northern Korean Peninsula,the intensity is V in great majority of this area except local area with intensity VI,and the damage is basically inaccordance with typical characteristics of corresponding intensity grade.In the southern Korean Peninsula,theintensity is IV in large part of the area,however,in some big cities such as Seoul etc.,not only high buildingsshook strongly,but also some people appeared perceptions such as feeling dizzy and so on,and electrical servicewas interrupted on one or two districts because of transformer tripping.These phenomena could be caused by theeffect of long-period wave generated from a large earthquake on far-field.     

国产高分影像在矿业城市生态安全性评价中的应用——以黑龙江省七台河市为例

为了实现矿业城市生态安全性评价,利用BJ2、GF1、ZY3等国产高分辨率卫星影像数据,采用遥感技术手段,基于GIS平台,构建景观安全评价体系。通过获取2017年度研究区内各土地资源类型分布现状数据,进行景观指数（破碎度、分离度、优势度、干扰度、脆弱度、生态风险度）计算,逐网格剖析后采用普通Kriging插值法（半变异函数）对研究区域的景观生态安全度进行定量分析与评价。结果表明：研究区内大部分地区景观生态安全处于中、中高和高水平,面积为538 951.58 hm²,占研究区面积的86.75%,呈现由矿产资源集中开采区向其外部、平原区向低山丘陵区安全等级逐渐升高,生态环境逐渐转好的趋势;低、中低安全区总面积为82 342.18 hm²,占研究区面积的13.25%,景观生态安全仍存在较大问题,需引起地方政府关注。     

皖南宁国一带印支期褶皱变形分析

】应用构造解析法,通过与褶皱变形有关的小构造研究,认为皖南印支期褶皱变形可分解为三期。它们的形态、方位各异,规模、强度不等,形成机制也不尽相同。它们之间相互叠加,形成了该区非常有特色的构造变形图案。     

Cryptic diversity and phylogeography of the island‐associated barnacle Chthamalus moro in Asia

Pleistocene glaciations were among the important historic events that shaped the population structures of marine organisms. Genetic studies of different marine fauna and flora have demonstrated the effect of Pleistocene glaciations on taxa that reside in marginal seas. However, how marine island species responded to Pleistocene glaciations remains relatively unstudied, especially in Asia. Genetic analyses based on the island‐associated barnacle Chthamalus moro collected from 14 sites in Asia reveal that C. moro comprises three distinct lineages, with COI divergence ranging from 3.9 to 8.3%. Population genetic analyses on respective lineages reveal signs of demographic expansion within the Pleistocene epoch at different times. The Ogasawara lineage, which has a more oceanic distribution, expanded the earliest, followed by the population expansion of the Ryukyu and Southern lineages that inhabit islands closer to the continent. The data suggest that the inhabitants of outer islands may have been less affected by Pleistocene glaciations than those that reside closer to the continent, as the former were able to maintain a large, stable, effective population size throughout the late Pleistocene.     

塔北古生界滨岸相混控碎屑岩体系沉积学和沉积模式

滨岸相混控碎屑岩沉积体系是指发育在滨岸带，受河流、波浪和潮汐混合水动力作用产生的复合碎屑岩沉积体系。受区域构造、物源、古地貌、海平面变化和滨岸水动力控制，塔里木盆地沙雅隆起区在志留纪—泥盆纪—石炭纪时期发育了辫状河三角洲、潮汐和波浪作用相互交替的滨岸相碎屑岩复合沉积体系。本文基于野外露头、钻井和测井等资料，开展了沙雅隆起区志留系—石炭系沉积层序、沉积相和沉积模式的综合研究，建立复合沉积体系的沉积学模式，包括：① 志留系—泥盆系的浪控- 潮控海湾沉积体系；② 下石炭统巴楚组的台地- 蒸发潟湖- 潮坪沉积体系；③ 下石炭统卡拉沙依组的河控- 浪控- 潮控三角洲沉积体系。下志留统柯坪塔格组滨岸滩坝和潮坪砂体、上泥盆统东河塘组冲积平原、海湾滩坝砂体和下石炭统卡拉沙依组辫状河三角洲砂体在塔北地区大面积分布，其冲积平原、三角洲前缘、水下分流河道砂体被后期潮汐和波浪作用改造后，形成潮汐水道砂体、河口坝砂体和滨岸滩坝砂体，物性条件明显改善，有利于形成优质储层区带。目前，滨岸混合水动力碎屑岩沉积体系已获得重大油气勘探突破，其沉积学模式可为塔北地区古生界碎屑岩油气勘探提供理论基础。     

纂修《文登市国土资源志》的几点做法

2007年6月25日,在文登市庆祝第17个全国“土地日”大会上,市委副书记王廷琦代表市委、市政府致辞,对文登市国土资源局编纂出版的《文登市国土资源志》和《海上仙山之祖——昆嵛山》画册大加赞扬,号召市政府各单位都要加强部门志的编纂工作。会后,来国土资源局索取志书和画册的部门领导络绎不绝,市内外看过志书的人士纷纷打来电话给予称赞和勉励,不少单位已决定编修志书,形成“方志热”。