粗唇鮠生物学的初步研究

１９９１年１０月至１９９２年７月，在嘉陵江下游采集粗唇标本２１１尾，进行了生物学性状的测量和统计运算．用胸鳍棘脱钙切片法鉴定年龄．体长与棘切片半径呈直线正相关．渔获物中８０％为２龄和３龄鱼，雌鱼的体重和肥满度均较同体长的雄鱼高．粗唇属一次性产卵的鱼类，产卵期为５～７月，雌鱼性成熟最小型为２龄，体长１０．６ｃｍ，体重２２．２ｇ．绝对繁殖力为１３７２（５８３～２３９２）粒，且与体长、体重、年龄和成熟系数成正相关。受精卵卵径２．０～２．２ｍｍ．强粘性．在２６．５～３０．５℃的水温下，经５０小时４２分孵出．初孵仔全鱼长５．２～５．８ｍｍ．     

冶勒电站库区水文地质条件的同位素研究

文章论述了四川冶勒电站库区内河水、泉水、承压水的同位素组成特征,讨论了泉水、承压水的补径排关系,确认了库区内河水和各层承压水之间不存在直接的水力联系,排除了河水向下渗漏的可能性。     

数理统计方法在测定脉图生理年龄中的应用

本文应用数理统计方法来研究人的生理年龄与人体脉图生理参数之间的关系.通过建立回归分析模型、进行显著性检验、选择最优回归方程等过程的原理,找出并论证了人的生理年龄同血压和各种脉图之间的相互联系.     

多光子解离CHClF_2富集~(13)C

用无氦TEA CO_2激光器(9μm带谱线)辐照F-22,选择性激发~(13)CHClF_2,使其达到离解,得到~(13)C的富集。测得选择系数α的峰值位置在1047cm~(-1),相对于~(13)CHClF_2的线性吸收峰位置红移了36cm~(-1),α随激光能量密度、F-22气压的增高而降低。     

On emplacement ages of lamproites in Zhenyuan County, Guizhou Province, China

Emplacement ages of lamproites that comprise lamproite and olivine lamproite in Zhenyuan County, Guizhou Province, China, have been constrained by the whole-rock Sm-Nd and Rb-Sr isochron methods and the whole rock K-Ar method. Intrusive activities of lamproites in the Sinantang area of Zhenyuan County, Guizhou Province, took place during the Late Cambrian, as indicated by the Sm-Nd isochron ages ( t ) = (503 ± 17) (2σ) Ma and by the Rb-Sr isochron ages ( t ) = (501.2 ± 4.6) (2σ) Ma. Intrusive activities of olivine lamproites at the Maping with Ⅱ-type diamond and Xitou in Zhenyuan County, Guizhou Province, took place from the Late Cambrian to the Early Ordovician, as evidenced by the Sm-Nd isochron ages ( t ) = (502 ± 27) (2σ) Ma and by the Rb-Sr isochron age ( t ) = (502 ± 27) (2σ) Ma. This suggests that the upwelling hot materials derived from the deep mantle were emplaced from the Late Cambrian to the Early Ordovician (503-497 Ma), while the time terminal of cooling of the geothermal event of magmatism-tectonism probably was at 442.64-435.54 Ma, as dated by the whole rock K-Ar method.     

Sm-Nd isotope dating of hydrothermal calcites from the Xikuangshan antimony deposit,Central Hunan

The research on Samarium-Neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit, Central Hunan, places precise timing constraints on the Sb mineralization in this area. It is revealed that the Xikuangshan deposit formed during the late Jurassic-early Cretaceous Period, the early- and latestage mineralization took place at (155.5± 1.1) Ma and (124.1±3.7) Ma, respectively. The accurate age determination of mineralization is very crucial for revealing the super-enrichment mechanism of the element Sb at the Xikuangshan mine, and lays some foundations for the further understandings of its ore genesis and mineralization mechanism.     

Carbon isotopic record of foraminifers in surface sediments from the South China Sea and its significance

Since the 1990s, the papers and data involved withthe South China Sea (SCS) have been emerging in largenumbers in the world as people pay more attention to thepaleoceanography of the SCS. There have been more than100 cores mentioned in papers containing p…