开展基建审计 服务台站综改

２００１年以来，根据省局党组安排，我们组织专人对部分县（市）台站综合设施改善项目进行了基建审计，取得了较好的社会经济效益。通过审计，在为台站节约开支的同时，锻炼了队伍，提高了审计人员业务素质，促进了被审单位的党风廉政建设。１拓宽审计领域，开展台站综合改善审计山西省１１９个基层气象台站中的绝大多数是５０、６０年代建成的。由于当时条件所限，基础设施和办公条件极为简陋，有的台站是由破庙改建而成，有的台站办公室和宿舍仅是几孔旧窑洞。经过风雨剥蚀，年久失修，变得更加破旧不堪。据综改前初步统计，全省基层气象…     

暗绿色硬质亚粘土层桩基的工程地质条件

本文重点叙述了离地表30米以内暗绿色硬质亚粘土层。此土层在上海地区分布较广,土质坚硬,常作为建(构)筑物的桩基持力层,文章从沉积环境、分布状况、土质特性及桩基承载力四个方面进行了分析探讨,並举实例说明。     

莫来铁尖晶岩的发现和玄武岩浆的深部分异作用

莫来铁尖晶岩是首次发现的一种新型火山岩,由铁尖晶石、莫来石、铁板钛矿和火山玻璃组成,其平均化学成分相当于一个简化的SiO_2-FeO~*—Al_2O_3三元系。莫来铁尖晶岩浆是原始岩浆深部分异的结果。原始玄武岩浆在地幔深处分离结晶出富含硬玉分子的斜方辉石、单斜辉石,进化岩浆向富Al、Fe而贫Si的方向演化,最终产生莫来铁尖晶岩浆。后者喷出地表,冷凝结晶形成莫来铁尖晶岩。     

石门县上五通石膏矿区水文地质条件及其作用浅析

石门县上五通石膏矿床是我省发现的大型优质石膏矿床之一。矿区水文地质条件比较简单,石膏矿体具有良好的隔水顶、底板,保存完整。但由于构造活动及地表风化作用的影响,矿层在地下水的作用下,其保存情况及矿石类型形成了明显的分带性。笔者以矿区水文地质条件为基础,将石膏矿的溶蚀带划分为淋滤带、溶滤水化带和水化带;并对矿区水文地质条件的成矿作用和地下水对早期形成的硬石膏矿床的改造和破坏作用进行了具体分析;提出了寻找隐伏石膏矿的水化学标志。这对研究石膏矿床的成因、指导找矿,以及加强矿山建设都是有益的。     

从滇黔桂“金三角”区域地层地球化学演化特征探讨卡林型金矿的物质来源

选用滇黔桂地区东经103°～110°,北纬22°～26°,面积约20万km2,34幅1∶20万水系沉积物统计结果资料,全面系统地探讨本区及其邻近区域地层地球化学特征及其与成矿的关系。结果表明:(1)与华南地区相比,本区存在Sb、As、Au、Hg等低温元素矿集区的地球化学块体,金具有深源性,而砷、锑、汞则是区域性的高背景,本区金与砷、锑、汞的相伴,既有必然性,又有偶然性;(2)与基性岩浆活动有关的亲基性场元素、氧化物、矿化剂高背景的形成,是本区右江裂谷带、富宁—关岭南北向断裂带、文山—富宁逆冲推覆构造带,特别是峨眉地幔柱所产生的基性岩浆喷溢及火山碎屑浊流沉积的客观地球化学反映;(3)黔西南地区二叠纪峨眉山玄武岩喷发导致二叠系和三叠系金及大量亲基性场元素的突变,右江裂谷活动至少始于寒武纪,随着时间的推移,由桂西往黔西南逐渐裂开;(4)滇黔桂"金三角"地区卡林型金矿的物源与裂谷、特提斯和区域性深大断裂和峨眉地幔柱长期活动相伴的基性火成岩及火山碎屑浊流沉积有关。     

Seismic characterization of basalt flows from the Faroes margin and the Faroe-Shetland basin

High‐quality seismic profiles across the Faroes volcanic continental margin and the adjacent continental shelf show contrasting styles of basalt emplacement across two major structural boundaries. At the rifted continental margin, the basalts form prominent seaward dipping reflector sequences up to 5 km thick. The same basalts, after they had travelled in a landward direction across the elevated, subaerial Faroes shelf, produced prominent landward dipping foresets, where they flowed across the paleo‐coastline into the deep water of the Faroe‐Shetland Basin. In both cases we are able to image details of the internal structure of the basalts as a result of using a low‐frequency airgun source capable of penetrating through the basalt sequence, together with long‐offset recordings from ocean bottom seismometers and a 12 km long, deep‐towed, hydrophone streamer.     

新疆北部晚石炭世至晚三叠世地壳热演化：——东准噶尔考克塞尔盖？…

在野外考察和室内研究的基础上,＾４０Ａｒ－＾３９Ａｒ定年揭示出新疆东准噶尔考克塞尔盖山前志留纪荒草坡群下组的主变质作用发生在石炭纪晚期,此后还受到了晚三叠世热事件的改造。结合区域地质资料,对新疆北部晚石岩世至三叠纪的地壳热演化进行了初步探讨。     

秦岭地区蚀变煌斑岩型金矿的发现及金的预富集研究

秦岭地区煌斑岩广泛分布,大部分蚀变煌斑岩型金矿发现于微成盆地南侧。本文对煌斑岩金的预集提出了认识,深入研究蚀变煌斑岩型金矿中金的预富集和成矿特征有望扩大在秦岭地区的找金前景。     

A Multiscale Vision Model applied to analyze EIT images of the solar corona

The large dynamic range provided by the SOHO/EIT CCD (1 : 5000) is needed to observe the large EUV zoom of coronal structures from coronal homes up to flares. Histograms show that often a wide dynamic range is present in each image. Extracting hidden structures in the background level requires specific techniques such as the use of the Multiscale Vision Model (MVM, Bijaoui et al., 1998). This method, based on wavelet transformations optimizes detection of various size objects, however complex they may be. Bijaoui et al. built the Multiscale Vision Model to extract small dynamical structures from noise, mainly for studying galaxies. In this paper, we describe requirements for the use of this method with SOHO/EIT images (calibration, size of the image, dynamics of the subimage, etc.). Two different areas were studied revealing hidden structures: (1) classical coronal mass ejection (CME) formation and (2) a complex group of active regions with its evolution. The aim of this paper is to define carefully the constraints for this new method of imaging the solar corona with SOHO/EIT. Physical analysis derived from multi-wavelength observations will later complete these first results. Supplementary material to this paper is available in electronic form at http://dx.doi.org/10.1023/A:1017579625208 with J.P. Delaboudinière P.I.