塔里木盆地轮南地区油气运移的路径、期次及方向研究

本文通过对塔里木盆地轮南地区及附近的钻井（出油井和未出油井）中揭示的裂缝，裂缝与成岩序列的穿插关系，连通砂体及断层和不整合面附近的矿物及矿物中流体包裹体研究，对塔里木盆地轮南地区油气运移路径和期次进行了探讨。通过研究指出了塔里木盆地轮南地区主要经历了3期大规模的油气运聚，地层之间的不整合面为油气横向运移的主要通道。高角度的裂隙及微裂缝为纵向运移主要通道。第一期油气运聚主要发生于海西期，第二期油气运聚主要发生在14－17Ma；第3期油气运聚主要发生在最近的5Ma以来。第一期油气运聚主要为自塔北隆起的西南，南向北，以横向运移为主；第二，第三期运聚主要自西南，南向北，自东向西运移，但主要以垂向运移为主。     

既有建筑地基基础加固劈裂注浆法在青纸汽运办公楼的应用

青纸汽运办公由于部分基础座落在松散的杂填土层上，产生不均匀沉降破坏，通过劈裂注浆加固，建筑物停止沉降，地基土承载力标准值提高了4倍，效果显著。加固劈裂注浆法是治理既有建筑地基基础沉降灾害的有效方法之一。     

未来10年我国不同生态区居民点建设占用耕地预测

通过以生态区为单位分析 ,预测 2 0 0 0～ 2 0 10年 10年间人口增长和居民点建设用地需求及其占用耕地面积。研究表明 :全国未来 10年人口净增加 12 6 96万 ,因人口增长造成的居民点建设用地需求 12 6 6 571hm2 ,其中占用耕地达 6 4 5545hm2 。耕地减少最多的是淮北平原、华北平原、长江下游平原、四川盆地丘陵、长江中游平原、闽粤丘陵平原、汾渭谷地等平原区。     

太原盆地东南部农村聚落空心化机理分析

在分析和界定空心化聚落的基础上 ,用雷达模型揭示了空心化聚落的激发因素和潜育环境 ;依据相对空化率和绝对空化率区位商构成 2× 2阶矩阵 ,将该区聚落划分为 4个空心化等级 ;并利用家庭预算曲线和地价理论 ,探讨了空心化聚落的成因机制 ;在研究聚落空间消长和应力状况的前提下 ,提出了反映聚落空心化的 5种过程模型 ,最后探讨了制止聚落空心化的若干措施。     

AFRICA IS COMING TO THE CAPE*

ABSTRACT. At the southern tip of Africa, culmination of one of the world'sgreat population shifts is there for the witnessing: a southward movement of Bantu‐speaking Black Africans, previously stalled in South Africa'sEastern Cape first by climatic factors and later by European‐imposed racial segregation. Cape Town, throughout its demographic history a “Coloured” and “White” city, is now Africanizing. Liberation from apartheid has brought rapid African influx, and the metropolitan population has more than doubled in less than twenty years. Sociocultural tensions and sociocultural possibilities ensue.     

Latent heat effects of the major mantle phase transitions on low-angle subduction

Very low to zero shallow dip angles are observed at several moderately young subduction zones with an active trenchward moving overriding plate. We have investigated the effects of latent heat for this situation, where mantle material is pushed through the major mantle phase transitions during shallow low-angle subduction below the overriding plate. The significance of the buoyancy forces, arising from the latent heat effects, on the dynamics of the shallowly subducting slab is examined by numerical modeling. When a 32-Ma-old slab is overridden with 2.5 cm/yr by a continent, flat subduction occurs with a 4–5 cm/yr convergence rate. When latent heat is included in the model, forced downwellings cause a thermal anomaly and consequently thermal and phase buoyancy forces. Under these circumstances, the flat slab segment subducts horizontally about 350 km further and for about 11 Ma longer than in the case without latent heat, before it breaks through the 400-km phase transition. The style of subduction strongly depends on the mantle rheology: increasing the mantle viscosity by one order of magnitude can change the style of subduction from steep to shallow. Similarly, an overriding velocity of less than 1 cm/yr leads to steep subduction, which gradually changes to flat subduction when increasing the overriding velocity. However, these model parameters do not change the aforementioned effect of the latent heat, provided that low-angle subduction occurs. In all models latent heat resulted in a substantial increase of the flat slab length by 300–400 km. Varying the olivine–spinel transition Clapeyron slope γ from 1 to 6 MPa/K reveals a roughly linear relation between γ and the horizontal length of the slab. Based on these results, we conclude that buoyancy forces due to latent heat of phase transitions play an important role in low-angle subduction below an overriding plate.     

临南地区石油运移方向与成藏期次研究

根据原油及油砂抽提物中含氮化合物分析、原油生物标志成熟度参数及储层流体包裹体烃类成分分析,研究了临南地区石油运移的方向、距离、成藏期次。结果表明临南油田仅有一期油气运聚成藏过程,属中新世末形成的成熟原油,4 甲基甾烷含量较高。曲堤油田存在两期油气运聚成藏过程,早期原油成熟度低,4 甲基甾烷含量低,运移距离较远,成藏后大部分散失 ;晚期充注的原油成熟度较高,4 甲基甾烷含量也较高,并保存至今。     

未来上海地区海平面上升对土压缩模量的影响分析

未来上海地区海平面上升将引起地下水位抬升，将会对土压缩模量E产生影响，Es是土的最重要的物理力学参数指标之一，尤其在地基沉降计算中具有重要意义。本文主要针对土压缩模量Es的预测分析工作，进行了地基变形的;探讨研究，供交流参考。     

周口电信枢纽楼基坑降水设计方案技术经济分析

通过分析两种不同的基坑降水设计方案，阐述了降水技术要求，并介绍周边建筑物不均匀沉降的防治措施。     

油罐地基不均匀沉降原因分析及纠偏加固处理方法

某油罐因地基发生不均匀沉降而倾斜，本文通过对油罐发生均匀沉降的原因分析，提出了倾斜油罐纠偏设计及地基处理方案，叙述了地基处理及纠偏施工方法，施工处理后经过半年的使用观察，效果良好。