浙江金衢盆地八十年代气候变化趋势及灾害演变特征分析

本文分析了本世纪八十年代金衢盆地的气候变化趋势。与前三个年代（五十、六十、七十年代）比较，八十年代具有变冷，少光，洪涝灾害频繁的趋势特征。同时，春季“三寒”（倒春寒、种田寒、５月寒），晚春初夏异常高温危害，夏凉，冬暖等异常现象突出。着重分析了气候变化及灾害演变对农林环境的不利影响，讨论了九十年代气候变异趋势及其对策。     

Soil Erosion Spatial Distribution Character of Sloping Field in the Sichuan Hilly Basin： Taking a Cultivated Slope in Neijiang as Example

0IntroductionNeijiang City locates in the south of The SichuanHilly Basin.The Sichuan Hilly Basin is underlainby horizontally bedded Mesozoic mudstones,siltstonesand sandstones.Purple soils developed on these rapidlyweathering rocks are widely distributed across the basin.According to second state soil erosion surveys based onremote sensing,the soil erosion rates in local area aretypicallyinthe range of3000-5000t·km-2·a-1[1,2].Inthe Sichuan Hilly Basin,one sloping field may is com-pose…     

珠江三角洲文化形态论纲

珠江三角洲文化形态的性质是务实求利;其特征是商业俗文化;其结构由岭南文化、中原文化、港澳文化和西方文化四因素构成;其地位是有中国特色的社会主义新文化的“曙光”,是中华民族大一统文化的“中介”。     

攀西裂谷中段摩挲营花岗岩的流动构造初析

本文通过对摩挲营花岗岩体的流动构造研究,查明了岩浆侵位时流动空间的形态。岩浆是以十多度的倾角沿安宁河断裂由北向南流动冷凝的。在岩体中,流动构造由定向排列的斑晶和包体显示出来。斑晶是石岩浆结晶的中晚期形成的,主要是由于受到岩浆流体内部的应力作用而定向;包体是岩浆中的固体岩块,它必然受到流体的改造和冲击,其形态特点能反映岩浆的流动特征。这对弄清地球深郜的动力学特点,查明岩浆的侵位机制及指导寻找与岩浆作用有关的矿床都有重大意义。     

Characteristics of carbonate gas pool and multistage gas pool formation history of Hetianhe gas field, Tarim Basin, Northwest China

<正> Hetianhe is a big carbonate gas field which isfound and demonstrated in the period of "Chinese NationalNinth 5-Year Plan". The proved reserve of Hetianhe gas fieldis over 600 ×10⁸ m³. Its main producing layers are Carbon-iferous bioclastic limestone and Ordovician carbonate com-posed of buried hill. The former is stratified gas pool withwater around its side, and the latter is massive gas pool withwater in its bottom. The gases in the gas pools belong to drygases with normal temperature and pressure systems. Basedon the correlation of gas and source rock, the gases aremainly generated from Cambrian source rocks. According tothe researches on source rock and structure evolution, andthe observations on the thin section to reservoir bitumen andthe studies on homogenization temperature of fluid inclu-sions, the gas pool has been identified and divided into threeformation periods. The first is Late Caledonian when the oilgenerated from the Cambrian source rocks and migratedalong faults, as a form of liquid facies into Ordovician carbonate res-ervoir and accumulated there. After that, the crustuplifted, the oil reservoir had been destroyed. The second isLate Hercynian when condensate gases generated from theCambrian source rocks and migrated into Ordovician res-ervoir, as a form of liquid facies. Since the fractures hadreached P strata, so the trap might have a real poor preser-vation condition, and the large-scale gas pool formation hadnot happened. The third gas reservoir formation period oc-curred in Himalaya. The fractures on both sides of Hetianhegas field developed violently under the forces of compression,and thus the present fault horst formed. The dry gases gen-erated from Cambrian source rocks and migrated upwardsas the form of gas facies into Ordovician and Carboniferousreservoirs, and the large gas pool as discovered at presentwas formed finally.     

塔里木盆地前震旦-石炭纪构造与地层组合特征

通过对塔里木盆地前震旦-石炭纪构造演化与地层组合特征的分析研究,将该盆地构造和地层系统划分为2大组合系统5个构造-地层组合.前震旦系为混合片麻岩、浅变质岩组成的地台基底,震旦纪发生板内裂陷形成坳拉槽,早寒武世-奥陶纪和石炭纪是盆地两次大的海侵期,沉积了富含烃类的碳酸盐岩建造,志留-泥盆纪为克拉通边缘隆升阶段,发育浅海相碎屑岩及碳酸盐岩建造.     

黄河沉积物中重金属离子的形态转化及释放研究

以黄河包头段上游清洁河段的沉积物为吸附剂,以Pb^2 、Cu^2 、Zn^2 、Cd^2 等多离子溶液为吸附质,开展了重金属离子被黄河沉积物吸附后的再释放,以及吸附作用对重金属形态转化的影响等实验研究．结果表明,重金属离子被黄河沉积物吸附后,各元素均不转入残渣态,Cu^2 和Zn^2 主要向碳酸盐结合态及铁锰氧化物结合态转化,Pb^2 主要向碳酸盐结合态和可交换态转化;Cd^2 主要转入可交换态和碳酸盐结合态．吸附后的赋存形态决定了Cd^2 的释放量及释放能力远远大于其它3种重金属离子,由Cd^2 排放引起的污染不易消除且影响长久．     

云南省金沙江流域生态环境建设的问题与对策研究--长江上游生态屏障建设重点地区调查报告之一

生态环境保护和建设是我国西部大开发的重要战略之一。云南省金沙江流域是长江上游生态脆弱地区,也是生态环境保护和建设的重点地区．在实地调研的基础上分析云南省金沙江流域地区的生态环境状况,探讨该区域生态环境建设中存在的主要问题,并提出了进一步加强该地区生态环境建设的对策建议．     

Geochronology of source materials from high-pressure and ultrahigh-pressure metamorphic rocks in Jurassic sedimentary rocks of Hefei Basin

Eclogite cobbles were discovered by Wang et al. (2001) in the Fenghuangtai Formation of the northern margin of Dabie Mountains in the Dushan area of Anhui Province, China[1]. They proposed that after the formation during the Triassic, the high-pressure (HP) and ultra-high-pressure (UHP) metamorphic rocks reached the sur-face through exhumation and uplifting before the late Ju-rassic. However, they have not provided any evidence about isotopic ages. One kind of cobbles of HP-UHP rocks w…