海口ZK26井多层位水温对比观测

在系统清理海口ZK26井3个不同层位(-153 m、-336 m、-510 m)近10年观测资料对比的基础上,对比单井多层位水温动态多年趋势、年、月、日动态类型,并对其不同动态类型的成因及影响因素进行分析.对比观测结果表明,海口ZK26井不同层位的水温表现出不同的正常动态特征,与观测层位的水文条件、水力性质有着密切的联...     

文化消费者对黄梅戏展演空间感知的模式与价值寻求：方法−目的链理论的应用

以安庆黄梅戏会馆和再芬黄梅公馆为例,基于方法?目的链理论模型,解读文化消费者对黄梅戏展演空间属性的感知评价、层次处理和价值导向的转变。研究发现：不同层次的空间属性在文化消费者的感知与体验中实现着新的组合与重构,由此形成了基于舞台展演内容、文化呈现形式以及演出环境氛围为主体的3种空间感知模式。结合文化消费者感知的心理结构与路径,黄梅戏展演空间被消费者建构为娱乐空间、情感空间和社交空间,空间的多元化意义和价值得到彰显。方法?目的链理论从消费者的感知与需求出发,探索文化空间意义生成路径,实现了文化空间与消费者之间的双向信息交换。     

新疆强震活动与环境因子预报

本文运用新疆历史地震资料,分析了该地区的强震时空分布及地震活跃周期和活动图象,并探讨了强震活动与空间环境因子的关系,这无疑对新疆强震活动趋势分析和该地区强震中长期预报具有较重要的意义。     

Relationship between Crustal 3D Density Structure and the Earthquakes in the Longmenshan Range and Adjacent Areas

Abstract: This paper presents the 3D density structure of crust in the Longmenshan range and adjacent areas, with constraints from seismic and density data. The density structure of crust shows that the immense boundary plane of density distribution in relation to the Longmeshan fault belt is extended downward to ~80 km deep. This density boundary plane dips towards the northwest and crosses the Moho. With the proximity to the Longmenshan fault belt, it has a larger magnitude of undulation in the upper and middle crust levels. Density changes abruptly across Longmeshan fault belt. Seismic data show that most of the earthquakes in the Longmenshan area after the 2008 Ms8.0 Wenchuan Earthquake occurred within the upper to middle crust. These earthquakes are clearly distributed in the uplifted region of the basement. A few of them occurs in the transitional zone between the uplifted and subsided areas. But most of the earthquakes distributes in transitional zone from subsided to uplifted areas in the upper and middle crust where relatively large density changes occurr The 3D density structure of crust in the Longmenshan and adjacent areas can thus help us to understand the pattern of overthrusting from the standpoint of deep crust and where the earthquakes occurred.     

钻孔摩擦灌注桩岩土设计参数取值商榷

桩周岩土极限摩阻力及其桩尖处岩土的容许承载力是公路工程钻(挖)孔摩擦灌注桩单桩竖向承载力计算的重要岩土工程设计参数,其取值是否适当事关工程安危和工程费用的经济合理.对此,工程勘察设计人员不仅应遵照<公路桥涵地基与基础设计规范>有关规定外,还应考虑场地地基岩土的地质时代、场地工程地质条件、岩土工程性质及有关因素合理取值,不可机械地依规范查表确定,这是岩土工程师应具有的最基本技能.     

Current Vertical Motion Analysis of Northwestern Margin of Ordos Based on Precise Leveling

Ordos block was squeezed by the Qinghai-Tibetan block and North China block, and the tectonic activity was intense. In the periphery of Ordos block, there was a series of folds zones and compressed faults with complicate structures. This paper used three-phase data of 1980,1990 and 2014 to calculate vertical velocity of Northwestern margin of Ordos and the analytical results indicated that ① the Hetao basin between the rise of Yinshan fault block and Ordos fault block showed relatively subsidence, in which Linhe basin was the most evident and the subsidence rate was about 2-4mm/a. The subsidence rate of Jartai -Yinchuan rift zone on the western margin of Ordos block was about 2mm/a; ② the whole testing zone exhibited the evident inherited movement characterized by mountain rise and basin subsidence; ③the two leveling section through the northern margin fault and Dengkou-Benjing fault showed that the difference between vertical velocities on two sides of the fault was less than 0.5mm/a.     

中国青藏高原深部地球物理探测与地球动力学研究（1958—2004）

经过半个多世纪的努力,中国学者在青藏高原进行的地壳上地幔地球物理探测工作取得了巨大进展. 累计完成长约45000km的深部地球物理探测工作,取得了许多科学数据,为探讨高原地壳上地幔结构、隆升机制和动力学研究奠定了基础. 为比较全面反映中国学者多年来的工作成果,作者广泛收集资料,总结了中国学者在青藏高原地壳上地幔地球物理探测工作程度,并按照方法分类绘制了系列工作程度图. 文中分别对地壳结构、上地幔的横向不均匀性、岩石圈的电性结构、青藏高原隆升机制、青藏高原地球动力学模型等几个方面所取得的主要成果做了概略的评述. 已有资料表明：青藏高原的莫霍面埋深变化较大,且在几条重要缝合带莫霍面两侧都有断错;根据目前的探测结果,高原在20±5km埋深范围内普遍存在壳内低速高导层,速度一般为5.6～5.8km/s,电阻率约为1～10Ω·m,厚度一般为5～10km,但横向分布不连续. 低速层与高导层的深度、厚度在趋势上一致,但不十分吻合.天然地震的研究结果表明,组成高原各个地块内部的地震各向异性方向大致相同,各地块的分界处各向异性方向往往有明显的变化;虽然对高原隆升机制还存在不同的看法,但至少认为高原是多期隆升、多种机制共同作用的结果这一点已达成共识. 综合已有的地球物理调查成果,结合地质地球化学资料建立的高原地球动力学模型,形象地表达出青藏高原岩石圈的双向挤压变形模式. 这些工作为研究青藏高原隆升和变形机制提供有价值的信息.     

南海中北部表层沉积物的矿物沉积

本文研究了南海中北部500多个样品的矿物学。认为,本区表层沉积物中矿物种类繁多,分布较为普遍,碎屑矿物(含火山物质)、粘土矿物、自生矿物常有出现。以前者为最显著(共60多种,其中重矿物50多种,轻矿物近10种),主要分布于陆架区及深海盆;粘土矿物次之,多分布于陆坡～深海盆;自生矿物较少,陆架～深海盆均有分布。文中根据矿物沉积特征和环境差异,把它划分为6个矿物区。     

Response of riparian vegetation to water-table changes in the lower reaches of Tarim River, Xinjiang Uygur, China

The lower reaches of Tarim River in the Xinjiang Uygur region of western China had been dried out for more than 30 years before water began to be diverted from Konqi (Peacock) River via a 927-km-long channel in year 2000, aimed at improving the riparian ecological systems. Since then, eight intermittent water deliveries have been carried out. To evaluate the response of riparian vegetation to these operations, the groundwater regime and vegetation changes have been monitored along the 350-km-long stem of the river using a network of 40 dug wells at nine transects across the river and 30 vegetation plots at key sites. Results show that the water table rose remarkably, i.e. from a depth of 9.87 m before the water delivery to 3.16 m after the third water delivery. The lateral distance of affected water table extended to 1,050 m from the riverbank after the fourth water delivery. The riparian vegetation has changed in composition, type, distribution, and growing behavior. This shows that the water deliveries have had significant effects on restoration of riparian ecosystems.