粤西合水、思贺地区花岗质岩石的成因

本区花岗岩的成因问题,存在着三种意见,作者根据区域地质调查获得的新资料,认为它是加里东期同构造花岗岩侵入体,主要依据是:它侵入震旦系云开群变质岩中,接触关系及界线很清楚;岩体有宽大的内部相和很窄的边缘相;岩体外围有角岩类组成的接触变质带。岩石具有同构造碎裂—花岗结构、片麻状构造,岩石化学成分稳定,据各种投影与图解结果,证明它属于岩浆型花岗岩。对晶形完好和浑圆状二种锆石,经分析其化学成分相同;采用 U-Pb法测定的年龄值,分别为469Ma 及461Ma,说明它们均形成时代基本相同。     

含金剪切带的地球化学特征

据 M·Bonnemaison 等人报道,含金剪切带的地球化学特征是由主要元素、示踪元素和探途元素组成:①主要元素开始产于围岩中,但金的矿化使这些元素的富集发生了变化;②示踪元素由矿化溶液带入,具有半区域矿化构造的特征;③探途元素局限在矿化带,反映了再活化和富集现象,构成了示踪剂。在法国Variscan 基底,砷总是产于含金剪切带中。这与横切加拿大魁北克卡迪拉克盆地的火山沉积岩的构造梧     

北半球冰川物质平衡变化的若干特征及其气候意义

根据北半球连续观测的４０多条冰川物质平衡资料，分析了目前冰川物质平衡状态及影响它们的地形因互。冰川物质平衡的变化在区域间存在着一定的联系：斯堪的纳维亚、落基山和天山地 区冰川物质平衡的变化在大多数时间内存在着对应联 系，而与阿尔卑斯山冰川物质平衡的变化具有不同程度的反向波动特征。     

湖南九峰山金矿点地质特征分析及找矿方向

九峰山金矿点是开展湖南紫云山地区矿产远景调查时新发现的矿点,通过对该矿点金矿化体分布范围、规模、形态、产状、含量及变化、矿石质量、结构构造及金矿化的控制因素等进行分析研究,初步总结了本区找矿标志,并提出今后工作的建议。     

甘肃小柳沟钨钼多金属矿田构造叠加晕浅析及找矿预测

通过对小柳沟钨钼多金属矿田地质地球化学特征及前人资料的综合研究,以小柳沟矿田中部祁青钼矿床4线构造叠加晕和深部成矿预测研究为重点,用围岩31件背景样品的几何平均值,为构造叠加晕分带提供地球化学背景依据;以小柳沟钨钼多金属矿单期次成矿原生晕轴向分带序列(自下而上)Cr、Co、Ni、V、Ti→W、Mn、Be、Sn、Bi、Mo、Cu→Pb、Zn、Ag→Au、As、Sb为基础,分析认为祁青钼矿4线构造叠加晕轴向分带序列(自下而上)Cu、Mo、Pb、Sb→As、Zn、Sn、Nb→Bi、V、Ti、Ba、Cr→Mn、W、B具"反分带"特征,且存在地球化学参数"反转"现象,指示成矿作用有叠加,预测深部存在第二成矿空间,钻探工程验证在祁青钼矿深部发现含钼隐伏花岗岩体,且岩体上部仍有石英脉型钼矿体,证实了构造叠加晕对深部找矿预测的有效性。认为小柳沟矿田深部斑岩型钼矿资源潜力较大,晚期花岗岩体凸起部位和外围分别是是寻找钼、中低温硫化物有关的铅锌矿床的有利地带。     

Status of two <Emphasis Type="Italic">Coreius</Emphasis> species in the Three Gorges Reservoir,China

Dam construction alters natural flow regimes which, in turn, cause significant changes in fish communities during and after impoundment. The construction of the Three Gorges Reservoir, from impoundment of the Changjiang (Yangtze) River, China, may have affected native fish species. Thus, the status of two lotic freshwater fish species, Coreius heterodon and C. guichenoti, were monitored in the Three Gorges Reservoir, including fish abundance, individual composition, growth, condition, and mortality. Data on both species were gathered from upstream, midstream and downstream areas of the reservoir and, where available, from studies published before and after dam construction. Lower abundance, slower growth, a less diversified age structure, poorer fish condition (indicated by hepatosomatic index) and higher mortalities were recorded in sites nearest the dam compared with upstream areas. Furthermore, after final impoundment, individual Coreius species inhabiting the area changed, with young individuals becoming more abundant, while upstream of the reservoir the two Coreius species became smaller at a given age. The results show that the status of the two Coreius species was subject to dramatic changes after impoundment.     

全新世早期弱夏季风事件的精确定位及机制探讨--以湖南莲花洞LHD5石笋为例

全新世早期是太阳辐射加强、全球温度上升,并伴随着冰盖消融的重要时期,而其间发生的冷事件以及亚洲季风区的弱夏季风事件的成因一直是全新世早期研究的重点。对亚洲季风-海洋-极地联系研究有着重要的意义。通过分析湖南莲花洞LHD5石笋28个U/Th年龄和535个氧同位素数据重建了全新世亚洲季风演化特征,其中全新世早期分辨率达8年。LHD5石笋记录到YD结束时间为11748±30 a B.P.,全新世开始于11684±39 a B.P.,转换时间约为64年,与格陵兰gicc05记录在误差范围内一致。LHD5石笋记录到全新世早期6次弱夏季风事件,事件年龄中心点分别为11461±34 a B.P.、10354±36 a B.P.、9957±25 a B.P.、9062±36 a B.P.、8744±23 a B.P.、8144±24 a B.P.,其δ18O值的波动幅度分别为1.08‰、0.94‰、0.66‰、0.90‰、0.55‰、1.02‰,这些弱季风事件在亚洲季风区具有普遍的区域意义。除8.2 ka事件之外,10 ka B.P.之前的弱季风事件除了受到太阳活动的影响,还受到北大西洋IRD事件的影响,而之后更多地受到太阳活动和ITCZ南移的影响。     

南岭科学钻探青白口系中发现381 Ma流纹岩

南岭科学钻探(NLSD-1)选址于江西省于都—兴国—宁都三县交界地区实施,构造上属华夏板块内部的武夷和罗霄两块体交汇部位。南岭科学钻探瞄准构造结合部区域地质问题和矿集区深部成矿预测两方面科学目标进行探索。NLSD-1开孔至1373.71 m揭露了连续的青白口纪地层,是一套完整的凝灰质火山碎屑岩韵律层,主要岩性有凝灰质粉砂岩、凝灰质细砂岩、变沉凝灰岩、凝灰质板岩和流纹岩。本次工作在科学钻探精细地质编录的基础上,对各类岩性地层进行镜下鉴定,并挑选流纹岩中的单颗粒锆石,应用LA-ICP-MS锆石U-Pb法进行定年,获得了一组高度谐和的同位素年龄,确定流纹岩成岩时代为381 Ma,为赣中南地区新元古代地层时代的进一步划分、归属和地质演化研究提供了新的信息。     

Morphological study of the genus <Emphasis Type="Italic">Herposiphonia</Emphasis> (Rhodophyta,Rhodomelaceae) on the coast of eastern Guangdong,China, with a description of <Emphasis Type="Italic">H. pinnata</Emphasis> sp. nov.

We present a taxonomic study of taxa of the red algae genus Herposiphonia (Rhodophyta, Rhodomelaceae), collected from the coast of eastern Guangdong, China. We made detailed morphological studies and considered recent taxonomic criteria for species delimitation, and are making the first report of five different species on the coast of Guangdong, including a new species. The species identified were H. caespitosa Tseng, H. hollenbergii Dawson, H. pecten - veneris (Harvey) Falkenberg, H. subdisticha Okamura and H. pinnata Ding and Tan sp. nov. H. pinnata sp. nov. is characterized by bright green thalli; most parts of the feathery thalli are free of the substratum; determinate branches and indeterminate branches are arranged in a chaotic sequence; the primary axis has bare segments; the determinate branch has 9–11 periaxial cells per segment; vegetative trichoblasts are abundant; and tetrasporangia are formed on the middle of the determinate branch with 1–8 successive segments in a single rectilinear series. This paper is also the first record of sporophyte plants of H. pecten-veneris.