CHIMEHERB中的有效成分对表皮细胞培养生长的影响

为观实CHIMEHERB有效成分,对新生小白鼠和人包皮外板的表皮细胞的生长影响,本文对7个实验浓度13次实验,112组592个组织块进行了组织培养的资料分析和机理的初步探讨,结果说明CHIMEHERB对表皮细胞无任何毒副作用,能100％的促进表皮细胞的生长.其相对生长率:小白鼠组为142.73％,人包皮外板组为440.58％,实验结果与临床应用效果一致.     

高速铁路和城市蔓延对雾霾污染的异质性影响

为了探寻高铁开通能否抑制雾霾污染以及这种抑制作用在不同城市空间形态下是否存在异质性,本文首先分析了高铁和城市蔓延对雾霾污染的作用机制,在利用LandScan数据测算2003-2016年中国281个地级市城市蔓延指标的基础上,采用动态空间面板模型检验了城市蔓延与雾霾污染的空间动态关系.借助双重差分(DID)模型验证了高铁...     

柴达木盆地自然伽玛曲线与古里雅冰芯记录的末次间冰期以来气候环 …

采用柴达木盆地达参１井井自然伽玛（ＧＲ）曲线进行古气候反演,分析了ＧＲ曲线记录的末次间冰期以来的环境变迁过程,表明ＧＲ曲线忠实地记录了构造运动及气候变化的影响,与古里雅产,格陵兰冰芯所记录的气候事件均能均较好对应,表明柴达木盆地同时包含了高原隆升和全球性气候变化的信息,是反映古气候变化良好的信息载体之一,是反映内陆干旱盆地环境与气候变化良好的代用指标。     

Evaluation of heavy metal contamination and implication of multiple sources from Hunchun basin, northeastern China

Present concentrations and distributions of heavy metals through profiles, surface soil, and stream sediment samples in the Hunchun area, north-eastern China, were investigated to determine the elemental background values. This study also aims to characterize potentially toxic materials such as pulverized fly ash (PFA) from power stations or ash and slag from coal used domestically in urban areas, agrochemicals applied inappropriately, and urban sewage sludges from Hunchun City, as well as to ascertain the possibility of natural enrichment through site characterization by mineralogical and geochemical investigation. The distribution of contaminants in the alluvial soils (fluvisol) of this area has been influenced by several interacting factors. The parent alluvial materials from weathered products of amphiboles have made coatings such as ferrihydrite, goethite, and hematite. This natural inheritance factor is supported by the fact that the concentrations of weak acid-extractable (plant-available) heavy metals are very low, except for Fe and Mn. However, in agricultural soils and adjacent stream sediments, an anthropogenic input of Cd, Pb, Ni and Cr by agrochemicals is strongly suggested. Also, F contamination by coal combustion and the dissolution of F-bearing minerals could cause some future problems. Wide distribution and significantly high concentrations of Cd, Fe, Mn, and F in soils throughout the combination of pollutants originating from lithogenic and the anthropogenic sources pose potential problems in utilizing water resources. Received: 14 June 1999 · Accepted: 27 December 1999     

福建省矿产资源潜力的地球化学预测

利用区域化探归面（水系沉积物测量）资料，使用区域浓度克拉克值及变化系数两个参数，对福建省32种元素的资源潜力进行了排序，认为在目前国家的导向矿种中，福建省的资源潜力依次为锌－银－铅－锡－金－铜－钼。同时根据谢学锦院士提出的地球化学块体学块体的理论和方法，预测了政和Au地球化学块体、龙岩中甲Cu地球化学块体、大田Pb地球化学块体的资源潜力，分别为金430吨、铜625万吨、铅408万吨。初步探讨了成矿系统的元素分带及地球化学模式研究的意义和方法，认为这项研究对上述地区的打矿突破具有重要作用。     

1995年日本兵库县南部地震时淡路岛上出现的地震断层的形态特征

1995年日本兵库县南部地震时在淡路岛上出现的地表地震断层主要由三条地表破裂带组成、野岛地震断层、松帆地震层和楠本地震断层。野岛地震断层从淡路岛北端的淡路町住西南延伸到一宫町的尾崎,长达18km,其北段沿着早期存在的野岛断层分布,而南段则作为新断层出现,野岛地震断层的断层的北段主要由一些相互平行或次平行的右列剪切断层和许多左列和性裂隙组成,其南段则是由集中在十多米宽的大量不连续的地表破裂带所组成。野岛地震断层一般走向N30°～60°E倾向SE,地貌错位和断层擦痕均显示出此断层为一具有逆断层性质的右旋走滑断层,沿一些主要露头测定的北段水平位移量一般为100～200cm,垂直位移量为5O～100cm;而南段的水平、垂直位移量均只有几厘米至20cm。最大位移量在平林断层崖测得;水平180cm、垂直l30cm、实际位移量2l5cm。松帆地震断层走向N40°～60°W,沿着淡路岛北端部的海岸线分布,长达约1km。楠本地震断层沿早期存在的楠本断层出现,分布于淡路岛东北部的海岸边上,走向N35°～6O°W倾向NW 。根据地表地震断层的形态及地貌错位特征,野岛地震断层可被分为四条断层段,并在形态上呈现右列。地质和地貌证据以及余震分布的特征清楚地表明这4条断层段的几何形态和分布特征是受早期存在的地质构造所控制的,同时也说明了地震断层的破裂过程具有拉分(pulling-apart)和推隆(pushing－up)的过程,这两个过程分别产生了张性裂隙、拉分盆地、逆断层和挤压隆起等构造。     

走滑拉分作用与相山产铀火山盆地的就位

相山火山盆地是我国著名的产铀火山盆地。本文依据相山盆地深部地质研究成果以及大陆动力学理论，探讨了相山产铀火山盆地的就位机制。研究表明，相山火山盆地火山活动划分为两个旋回，其就位受制于区域深断裂的走滑拉分作用。即第一旋回的火山机构就位于NE向深断裂右旋走滑复活产生的EW向拉分构造，形成了东西向展布的裂隙式火山喷溢带；第二旋回的火山机构就位于NE向深断裂左旋走滑复活产生的SN向拉分构造与EW向基底断裂的结点，产生了中心式火山岩浆喷溢侵出。此外，还探讨了富大铀矿的形成机制。     

Petrogenesis and sedimentary environment of silicate in Late Paleozoic in Kala area of Western Sichuan Province

In order to study the sedimentary environment characteristics of the Late Paleozoic in Kala area of Western Sichuan Province, the authors have conducted the petrological and geochemical analyses of the widely distributed silicate in Qiongyi Formation of Lower Carboniferous and Kawenggou Formation of Upper Permian. The results show that the silicate in the study area belongs to the pure siliceous rocks, with a continuous supply of land-based materials during the deposition process. The average Al/(Al+Fe+Mn) ratio is 0.62, and the silicate shows a biogenic origin by the Al-Fe-Mn diagram. The ratios of Al₂O₃/ (Al₂O₃+ Fe₂O₃), Th/U, Th/Sc, (La/Ce)_N and (La/Yb)_N and tectonic environment discriminant diagram demonstrate that the silicate developed in a shallow-slope depesitional environment in the continental margin. The Ce_anom value is -0.04 to 0.07, and it gradually increases from the Carboniferous to the Permian period, indicating the water body is in an anoxic environment with gradually increasing reducibility. The Garz--Litang basin opened in the Carboniferous period, in accordance with the regional geological evolution, and it continued to expand during the Permian period, with the gradually increasing depth of the seawater within the sedimentary basins.     

闽西南永定大坪辉长岩脉的年代学、地球化学特征及地质意义

南岭地区湘南-赣南-粤北-闽西南近东西向的岩浆岩活动带在年龄、成因、动力学背景等方面一直存有争议.以福建西南部永定地区的大坪辉长岩脉为研究对象,在详细的野外工作及镜下岩相学观察的基础上,对其开展了斜锆石U-Pb同位素定年、全岩主微量元素含量以及Sr-Nd同位素比值的测试工作.获得同位素年龄为184.0±6.5 Ma,表...