广西西湾煤系首次发现牙形刺及其地层意义

西湾煤系是广西重要含煤层位之一,以碳酸盐岩夹煤层为特征,自下而上分天堂组和大岭组,主要煤层赋存于大岭组中。煤系时代有晚三叠世与早侏罗世之争。1988年笔者之一冯少南,曾报道了天堂组产植物化石Danaeopsis fecunda Halle,为煤系时代归属提供了重要古生物依据。今年笔者在大岭组的灰岩中分析出牙形刺,认为大岭组的时代应属晚三叠世,并进一步说明大岭组为潮坪泻湖→滨海沼泽相沉积。     

菏泽市土地开发整理可持续发展研究

该文分析了菏泽市土地利用现状及存在的问题,认为现阶段菏泽市土地整理应以农用土地整理为主,重点放在农村地区,对土地开发整理规范化管理是当前土地整理发展的方向。因此,菏泽市加大土地开发整理力度,科学利用本地特色资源,监管得力,缓解了该市土地资源的紧张状况,有利于土地资源的规范化发展,确保了经济的可持续发展。     

Hematological changes in white spot syndrome virus-infected shrimp, Fenneropenaeus chinensis (Osbeck)

The pathological changes of hemocytes in the haemolymph and hepatopancreas were examined in experimentally and naturally WSSV (white spot syndrome virus) infected Fenneropenaeus chinensis. The results showed that the pathological manifestations of hemocytes were similar among moribund shrimps infected via injection, feeding and by nature. Firstly, the total hemocyte counts (THCs) in WSSV-infected shrimp were significantly lower than those in healthy shrimp. Secondly, necrotic, broken and disintegrated cells were often observed, and a typical hematolysis was present in the haemolymph smear of WSSV-infected shrimp. Thirdly, necrosis and typical apoptosis of hemocytes were detected with TEM in the peripheral haemolymph of WSSV-infected shrimp. Hyalinocytes and semi-granulocytes with masses of WSSVs in their nuclei often appeared, whereas no granular hemocytes with WSSV were found in the hepatopancreas of moribund infected shrimps. All our results supported that hemocytes were the main target cells of WSSV, and hyalinocytes and semigranular hemocytes seemed to be more favorable for WSSV infection in F. chinensis.     

基于弧段标记的交通网络时间最短路径算法

标号算法是经典的最短路径算法之一,在交通领域中具有广泛的应用。在交通领域中,时间最短路径比距离最短路径更有意义,而时间最短路径不仅与道路的时间权值有关,还与道路之间的转弯阻抗有关。在传统的交通路网抽象方式下,道路抽象为平面图中的弧段,道路间的交叉口抽象为节点。本文介绍了一种适用于传统交通路网模型的弧段标记时间最短路径算法,详细阐述了该算法的原理、数据基础与运行结构。通过分析和实例测试表明,该算法可以顾及城市路网在路口的交通限行与转弯延迟的影响,并且时间复杂度低,具有一定的实际应用价值。     

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用区域重力资料确定的华北地台南缘地缝合线及其地质意义

利用１∶２０万区域重力资料，结合航磁，电磁测深、遥感、天然地震等丰富的地质、地球物理资料，根据断裂的地质、地球物理标志，在华北地台南缘发现并确定了控制火山喷发的裂隙—中心式古火山通道，即隐伏的北西西向的上戈—铁炉坪—付店超壳断裂带。该断裂属华北地台南缘不同时代、不同性质的近东西向的地缝合线。研究认为：该断裂及其次级断裂不仅是重要的长期多次活动的控岩、导矿和容矿构造，而且也为矿床的多次改造、叠加和再富集提供了热源。它的发现，对重新认识豫西地区大地构造的演化特征，建立新的成矿模式，拓宽该区的找矿前景具有重要意义。     

A STUDY ON REGIONAL DIFFERENCE OF CHINA＇S PAID URBAN LANDUSE SYSTEM AND GRADING

董黎明，李向明，冯长春ＡＳＴＵＤＹＯＮＲＥＧＩＯＮＡＬＤＩＦＦＥＲＥＮＣＥＯＦＣＨＩＮＡ＇ＳＰＡＩＤＵＲＢＡＮＬＡＮＤＵＳＥＳＹＳＴＥＭＡＮＤＧＲＡＤＩＮＧ￥ＤｏｎｇＬｉｍｉｎｇ；ＬｉＸｉａｎｇｍｉｎｇ；ＦｅｎｇＣｈａｎｇｃｈｕｎ（ＰｅｋｉｎｇＵｎｉ...     

Lake retreat in the Qinghai-Xizang plateau with additional reference to its climatic significance

The author made an approximate dating of the highest shorelines of the three larger interior lakes and proved that during late Q₃ or early Q₄, there existed a higher lake level in the plateau, reflecting that the climate then was much more moist than it is today. It could be presumed from a study of these two ages that such higher lake levels correspond with both the last glacial epoch (i. e., the latter half) and the lowest sea level of the East China Sea then. Moreover, interpretations of aerial photos and an on-the-spot survey revealed that since then these lakes had 8–10 rhythms of retreat, indicating that the climate in central Asia and the plateau at that time had 8–10 comparatively arid periods. As the plateau is still in the faster process of upheaval, it is expected that on a longterm basis, the climate in this region will tend to be continuously dry. However, should there be a neo-glacial epoch in the world, and if the higher lake level really corresponds to the glacial epoch, then in the not distant future, the lake level will possibly rise again to some extent. Thanks are due to the No. 2 Institute of Oceanography of SOA for its analyses of C¹⁴ dating specimens. This paper was published in Chinese inOceanologia et Limnologia Sinica 17(3): 207–216, 1986.     

太湖水污染扩散插件式模拟系统

插件式太湖水污染扩散模拟系统,基于三维水体污染扩散模型,结合GIS技术和三维可视化技术,再现了水体污染物运移扩散的时空分布特征与动态演进过程.为了保证系统的可扩展性,需要一种松散的耦合机制.插件技术可以有效地降低系统功能模块间的耦合,把插件技术引入GIS的二次开发可以赋予系统动态可扩展性.本文首先,介绍插件式系统的一般...     

南华北盆地青白口系—侏罗系层序界面时空分布特征研究

以位于秦岭—大别造山带之北、华北陆块南部、地跨华北陆块稳定块体、陆块南部边缘变形带的南华北盆地为研究对象,通过对研究区42条不同时代的野外剖面详细观测,运用层序地层学理论,把南华北盆地作为一个整体系统,对青白口系—侏罗系层序界面特征及时空分布规律进行了系统分析,共识别出了8种类型层序界面的物质表现形式,分别是不整合面、渣状层、古喀斯特作用面、冲刷侵蚀面、超覆面、岩性岩相转换面、最大海泛面、最大湖泛面。并重点讨论了各类型界面的时空分布特征。结果表明:在时间演化上,从早到晚由海相—海陆过渡相—陆相,层序界面经历了海相沉积不整合、古喀斯特作用面、渣状层到陆相不整合面、冲刷侵蚀面等;在空间上,同一层序界面在不同相带表现形式不同,同一种类型的界面可在不同相带出现,但不同相带表现特征有一定差异性。