晚新生代元谋盆地演化与河谷发育研究

元谋盆地是在晚新生代青藏高原与云南高原隆起过程中形成的众多断陷盆地之一,流经元度盆地的龙川江和金沙江。其河谷发育与盆地演化具有密切关系,通过对元谋盆地及其邻区的层次地貌与相关沉积的分析研究,认为,始新世晚期￣中新世晚期是夷平面形成时期,中新世晚期￣３．４０ＭａＢＰ前后是第一级剥蚀面形成时期;元谋盆地形成于３．４０ＭａＢＰ前后第一级剥蚀面解体过程中,其后盆地经历了３．４０￣１．７８ＭａＢＰ的古湖形成     

黄土高原晚第三纪红土的形态学和地球化学特征及其环境指示意义

对甘肃西峰地区晚第三纪红土和第四纪风成典型黄土的化学元素、矿物组成和矿物颗粒形态特征研究揭示出，该区红土下部（６．２ＭａＢ．Ｐ．前）是红化的土壤物质与其它物质一起经流水搬运再堆积的产物；中部（６．２Ｍａ～３．４ＭａＢ．Ｐ．）未发现再搬运的痕迹，是风尘堆积经风化和间歇性地下水位波动作用所形成的；上部（３．４～２．６ＭａＢ．Ｐ．）是典型的风尘堆积－土壤序列。由于干旱区的存在是黄土高原风尘堆积的前提条件     

青藏高原：全球气候变化的驱动机与放大器──Ⅰ 新生代气候变化的基本特征

除周期性气候波动外，新生代气候变化的基本特征是阶梯状气候变冷、波动幅度的不断增加和气候波动周期的转变。深海氧同位素记录表明新生代曾发生至少三次快速变冷事件，它们分别发生在３６，１５和２．４ＭａＢＰ前后。根据来自北大西洋的深海氧同位素记录，第四纪气候变化的趋势是波动幅度增加、频率降低。Ｂ／Ｍ界限附近，气候波动周期由４１ｋａ转变为１００ｋａ。黄土高原上黄土地层与磁化率研究揭示，现代东亚季风出现于２．４Ｍａ前，并于１．１和０．６ＭａＢＰ前后两度加强，现在的季风环流形势形成于０．６ＭａＢＰ，米兰柯维奇理论不能解释上述新生代气候的阶梯状变冷、第四纪气候的阶段性和东亚季风的形成及加强，因此除轨道因素外，还有别的因素控制气候变化。     

青藏高原：全球气候变化的驱动机与放大器──Ⅱ．青藏高原隆起的基本过程

４０Ｍａ前印度板块与欧亚板块的碰撞导致了特提斯海的封闭和西藏成陆，但４０～２０ＭａＢＰ间地面很低。２０Ｍａ前的构造运动使青藏地区一些山地隆起，但而后又经历了长期的夷平，地貌与生物证据揭示，早上新世高原的高度仅约１０００ｍ。高原的强烈隆起开始于３．４Ｍａ前，这被高原内外普遍的砾岩堆积和盆地演化记录了下来。青藏高原东部盆地演化与大河流发育研究表明，至少有１０次强构造上升事件发生，它们分别开始于３．４、２．５、１．７、１．３、１．１、０．８、０．６、０．１４、０．０５和０．０１ＭａＢＰ。其中２．５、１．１、０．８、０．６和０．１４ＭａＢＰ五次上升事件对高原隆起十分重要。     

黄山山体的演化过程研究

本文指出黄山区褶皱运动不是在印支放因而是在燕山旋回中期，与黄山花岗岩浆侵入同步，发生子１２５Ｍａ左右．花岗岩体经长期缓慢上升和剥蚀作用于距今３０Ｍａ（渐新世中期）时形成了黄山顶部光明顶期夷平面．距今５Ｍａ（上新世）时形成了黄山第二层地貌面－老人峰期剥蚀面．第四纪初（距今约２．５Ｍａ）的喜马拉雅旋国第三幕时，该区花岗岩体呈断块大幅度抬升，使现代的黄山正处于青年期中山峡谷阶段．依据地貌特征、堆积物分析、孢子花粉组合、气候特征以及山顶上奇峰巧石等证据，表明黄山第四纪时期没有经历过冰川作用，黄山顶部仅遭受了寒冻作用．     

碱土云母可切削玻璃陶瓷的研究

基于Ｂａ０．５Ｍｇ３（Ｓｉ３ＡｌＯ１０）Ｆ２－Ｍｇ２Ａｌ４Ｓｉ５Ｏ１８－Ｃａ３（ＰＯ４）２系统，制备出了含Ｂａ碱土云母为主晶相的可切削玻璃陶瓷，弯曲强度σｂ＝２２９ＭＰａ，断裂韧性ＫＩＣ＝２．４８ＭＰａ．ｍ＾１／２，钻孔速度大于７ｍｍ／ｍｉｎ。优良性能的获得借助于Ｂａ云母玻璃陶瓷可控的微观组织，即相互交错的云母晶体和“卷心菜”的组织特征。     

UO2（PMBP）2HMPA配合物的合成与结构研究

合成了ＵＯ_２（ＰＭＢＰ）_２ＨＭＰＡ（ＰＭＢＰ＝１－苯基－３－甲基－４－苯甲酰基－吡唑啉酮－５，ＨＭＰＡ＝六甲基磷酰胺），测定了该配合物的元素组成、红外光语、质子核磁共振谱及晶体结构。该晶体属于单斜晶系，空间群为Ｐ２_１，ａ＝１．１４６８（５）ｎｍ，ｂ＝１．４７７７（２）ｎｍ，ｃ＝１．４０５６（６）ｎｍ，β＝１００．９１（４）°，Ｖ＝２．３３８９ｎｍ￣３，Ｄ_ｃ＝１．４３ｇ／ｃｍ￣３，Ｚ＝２，Ｆ（０００）＝９７９．８５。在配合物中，Ｕ原子采用七配位，其配位多面体为扭曲的五角双锥。     

某些添加剂对Ti／PbO2电极上ClO4^—离子阳极形成过程的影响

本用分解极化曲线法研究了某些添加剂对Ｔｉ／ＰｂＯ２电极上ＣｌＯ４＾－离子阳极形成过程的影响，研究结果表明，Ｆ＾－，ＣｌＯ４＾－，ＢｒＯ３＾－，Ｂ４Ｏ７＾２－，Ｂａ＾２＋等离子均使ＣｌＯ４＾－的阳极形成电流效率提高，而Ｃｒ２Ｏ７＾２－，Ｓ２Ｏ８＾２－，ＳＯ４＾２－，ＭｏＯ４＾２－，ＩＯ４６－，Ｐ２Ｏ７＾４－，Ｆｅ（ＣＮ）６＾４－，Ｃａ＾２＋和Ｍｇ＾２＋等离子均使电流效率降低，根据假设的机理讨论了使     

动物体液中的胞外钙调素结合蛋白（快报）

利用以生物素标记钙调素为探针的凝胶覆盖技术检测动物体液中胞外钙调素结合蛋白（ＣａＭＢＰ）。结果，人的唾液中检测到至少３种分子量分别为１４ｋＤ，２４ｋＤ和５２ｋＤ的ＣａＭＢＰｓ。其中，５２ｋＤ蛋白与ＣａＭ的结合依赖于Ｃａ２＋的存在，而２４ｋＤ和１４ｋＤ蛋白则不依赖于Ｃａ２＋。在鸡血清里，检测到以９４ｋＤ，４４／４５ｋＤ蛋白为主的４～５种胞外ＣａＭＢＰｓ，所有的这些蛋白与ＣａＭ的结合都依赖于Ｃａ２－。此外，在牛奶中也检出胞外ＣａＭＢＰｓ。以上结果，证明了在动物中普遍存在胞外ＣａＭＢＰｓ，为胞外钙调素的作用机理提供了新线索。     

饱和一元醇物理化学性质的定量探讨

拓扑指数ｘｚ、路径数ｐ１和ｓ１、ｓ２是表征饱和一元醇分子大小、支化度、形状和羟基位置等结构特征的重要参量．本文提出计算饱和一元醇物理化学性质Ｐ的定量公式为：Ｐ＝ａ０＋ａ１ｐ１＋ａ２ｘ２／３ｚ＋ａ３ｓ１＋ａ４ｓ２式中ａ０、ａ１、ａ２、ａ３和ａ４为系数,对于某一物理化学性质为一定值．本文预测了含１０个碳原子以内的饱和一元醇的原子化热ΔＨａ、气相生成热ΔＨｇｔ、摩尔折射Ｒｍ、蒸发热ΔＨｖ、摩尔磁化率ＸＭ、液体密度Ｄ２０４、沸点Ｂ．Ｐ．、保留体积ｌｏｇＶｇ和分配系数ｌｏｇＰ等９项物理化学性质．     

巧家盆地河流沉积与重矿物特征对金沙江贯通的指示

通过对云南巧家盆地第四纪河流沉积和重矿物特征的研究,探讨金沙江下游巧家段水系的发展和演化过程。研究结果表明:1.6 Ma B.P.之前巧家盆地开启后,古金沙江巧家段南流水系也随之形成,并在盆地内发育了至少3期河流沉积,当时为宽阔的辫状河沉积环境,物源区位于巧家以北至四川西昌-昭觉一带的黑水河和西溪河流域,河流将玄武岩、灰岩、砂岩等砂砾携带至盆地中堆积,重矿物组合为锆石-绿帘石-金红石-电气石-角闪石-磷灰石;在0.5 Ma B.P.之前,由于云南高原的隆升使得古金沙江巧家段水系南流受阻,并在古水系支流的溯源侵蚀下被袭夺,造成巧家河段的倒转北流,金沙江贯通,巧家段水系物源区发生巨大变化,河流开始将金沙江中上游流域的板岩、千枚岩、片岩以及石英岩等砂砾带至盆地,重矿物类型中也开始出现石榴子石,在构造活跃期河流不断向西迁移并进行下切,形成了金沙江4级阶地。巧家盆地河流沉积与重矿物特征及相关年代的研究显示,巧家段水系的袭夺倒流,金沙江的贯通应发生于0.5 Ma B.P.之前。     

Discovery of a 1.0 Ma Yellow River terrace and redating of the fourth Yellow River terrace in Lanzhou area

Based on the aeolian loess sequence-stratigraphic division and paleomagnetic datings on terraces, we found that an undiscovered terrace with the age of 1.0 Ma BP lies between the Dunwashan terrace and Wuyishan terrace. This terrace recorded an intensive Yellow River incision event during that period. Results of paleomagnetic dating and optically stimulated luminescence (OSL) dating of the Wuyishan loess section and Zaoshugou loess section on the fourth Yellow River terrace (T4) show that the age of the fourth Yellow River terrace in Lanzhou area is 0.86 Ma BP rather than the previously believed 0.6 Ma BP. This result answers a long-term question in the geomorphology community of whether there exists a 0.8 Ma terrace in Lanzhou area. The discovery of the 1.0 Ma Yellow River terrace and redating of the age of 0.6 Ma terrace in Lanzhou area provide new insights into further research on the evolution of Yellow River.     

Discovery of a 1.0 Ma Yellow River terrace and redating of the fourth Yellow River terrace in Lanzhou area

Based on the aeolian loess sequence-stratigraphic division and paleomagnetic datings on terraces, we found that an undiscovered terrace with the age of 1.0 Ma BP lies between the Dunwashan terrace and Wuyishan terrace. This terrace recorded an intensive Yellow River incision event during that period. Results of paleomagnetic dating and optically stimulated luminescence (OSL) dating of the Wuyishan loess section and Zaoshugou loess section on the fourth Yellow River terrace (T4) show that the age of the fourth Yellow River terrace in Lanzhou area is 0.86 Ma BP rather than the previously believed 0. 6 Ma BP. This result answers a long-term question in the ge-omorphology community of whether there exists a 0. 8 Ma terrace in Lanzhou area. The discovery of the 1. 0 Ma Yellow River terrace and redating of the age of 0.6 Ma terrace in Lanzhou area provide new insights into further research on the evolution of Yellow River.     

山西临猗杨范第四纪沉积剖面初步研究

通过对杨范剖面黄土地层岩性特征、沉积结构、质量磁化率和频率磁化率的分析及与深海氧同位素曲线的对比,划分了剖面地层,初步确定了黄土沉积始于1.20 Ma B P,黄土沉积以来该区发生了13次大的干冷-暖湿气候变化;沉积转型指示河流强烈加积转变为河流侵蚀,代表约在1.20 Ma B P发生过一次强烈的构造抬升事件。     

Paragenesia of Quaternary pediments and river terraces on the north piedmont of Wutai Mountains

A study has been made of the paragenetic relations of the pediments and river terraces on the northern piedmont of Wutai Mountains via geomorphologic mapping of 1:10000 scale, and an analysis on the role of tectonic, climatic, and drainage factors in the parageneses. The Quaternary pediments and river terraces on the north piedmont of Wutai Mountains united to constitute six steps of geomorphic surfaces. The episodic uplifting of fault blocks was the dominant factor in the formation of the unified surfaces, however climatic change and drainage diversities led to undulation of the surfaces. The second terrace of Yangyan River (T2) was formed in the last glacial maximum, when the river was in aggradational state. The third to fifth terraces were formed in interglacial stages, when the river was in equilibrium or degradational state. It is inferred that climate had no insignificant effect on the river incision caused by tectonic uplifting. In light of terraces dating, since the Quaternary the Wutai fault-block mountains experienced six rapid uplifting events, and the starting time of the last four events was respectively 1.2, 0.6, 0.13, and 0.02 Ma B.P.     

Paleomagnetic dating of the topmost terrace in Kouma,Henan and its indication to the Yellow River''''s running through Sanmen Gorges

How did the Yellow River develop and evolve? Whendid it form? The geoscientists have concerned these im-portant questions for a long time. They have done a lot ofresearches on these issues and gotten a lot of valuableresults, while there are still many controversies. In general,it mainly includes several points as follows. According tothe transition of the fluviolacustrine strata, biological fos-sils and geologic structure in Lanzhou and Yinchuan, Linmade a conclusion that the Yellow River…     

Paleomagnetic dating of the topmost terrace in Kouma,Henan and its indication to the Yellow River＇s running through Sanmen Gorges

In the east of Xiaolangdi, many river terraces are developed at the exit of the Yellow River Gorges. Among them the terraces in Kouma, Yanshi of Henan Province are most typical, where the Yellow River developed three staircase terraces, among which the altitude of gravel stratum of the topmost terrace is 30-35 m higher than the river level.The top of the gravel stratum was covered by 60 m eolian loess deposits which have many brownish-red paleosol strips.And the paleosol $14 is at its bottom. Research on systematic magnetostratigraphy and paleosol-loess matching indicates that the bottom age of the loess on the topmost terrace is 1165 ka. Therefore, it can be concluded that the terrace develops no later than 1.165 Ma and the situation that the Yellow River runs through Sanmen Gorges and inpours into East China Sea happened at least before 1.165 Ma.     

Terrace dating as an archive of the run-through of the Sanmen Gorges

Analysis of morphological properties in the Sanmen Gorges region of the Yellow River shows that four river terraces have been developed at the entrance to the gorges. Commonly, thick aeolian loess-paleosol sequence was deposited on the terraces, which makes it easy to date the terraces. The dating of paleomagnetic, loess-paleosol sequence matching and thermoluminescence show that terraces T₂, T₃ and T₄ were formed 0.129 Ma, 0.625 Ma and 0.865 Ma ago, respectively. The formation of these terraces in this region indicates that the Yellow River has experienced four intensive downcutting events during the last 0.9 Ma. The Yellow River cut through the Sanmen Gorges and inpoured into the East China Sea no later than 0.865 Ma.     

黄河山陕峡谷保德-克虎段高阶地砾石层的初步研究

野外考察发现山西黑峪口地区存在七级阶地序列,其中上覆红粘土的T6、T7阶地为晚第三纪阶地.对该区阶地上砾石的岩性和粒径进行了研究,岩性对比表明,T6、T7阶地上砾石的岩性与黄河低阶地上砾石的岩性相似,而与东西向的蔚汾河阶地岩性差别较大;上下游之间对比发现,灰岩砾石岩性由保德地区占主导地位到克虎地区退居次要地位,灰岩砾石的粒径也从上游向下游变小,说明该区晚第三纪阶地并非东西向河流形成的,而是古黄河或古南北向水系的产物.T7阶地上覆盖厚度70m以上的粉、细砂层和晚第三纪红土层,磁性地层研究表明,该层的底部时代在6.8Ma左右,T6阶地上覆红粘土的底部年龄在3.3Ma左右,山陕峡谷由北向南流的古河流在6.8Ma之前已经形成,T6阶地的形成时代与青藏运动A幕相对应.青藏运动A幕以来河流在该区下切了160m,平均下切速率约为青藏运动A幕以前平均下切速率的5倍以上.