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。     

Analysis on Landscape Ecological Risk of the Qinghai-Tibet Plateaus：A Case Study on Niyang River Basin

0IntroductionWhether the regional ecosystems are securityis determined from two aspects which arethe ecological healthandthe ecological risk.Ecologi-cal riskreferstothe sufferedinterferences and disas-ters of ecosystems,and the damaged possibilities ofecosystems structures andits function.The relation-ship betweenecological riskandecological securityisinverse function.Therefore,the analysis of regionalecological riskis ani mportant aspect of studying onecological health,which can provide plann…     

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…     

塔里木盆地大中型油气田形成及分布规律

目的 探讨塔里木盆地油气藏形成及分布规律,为油气田勘探部署提供依据。方法 运用石油地质综合研究方法,探讨了区域构造背景,有效烃源岩分布及其成熟度、储盖组合、后期构造变动等对塔里木盆地大中型油气田形成及分布的控制作用。结果 塔里木盆地油气分布十分复杂,油气藏形成及分布受多重因素控制;早期形成、长期继承发育的大型稳定古隆起及其斜坡以及前陆逆冲带第2,3排构造分别是大中型油气田形成的最有利地区;古隆起控油、斜坡富集以及隆起高部位油气易发生调整、斜坡部位有利于保存,是克拉通区油气藏形成和分布的重要特点;已发现的油气藏具有多期成藏、晚期调整的特点,早期形成的原生油气藏后期特别是晚喜山期普遍受到了调整改造,以克拉通区海相油气藏最为突出;保存条件对塔里木盆地油气藏形成与分布具有重要控制作用,特别是优质区域盖层的存在,是大中型油气田形成和保存的关键。结论 继承性古隆起与隐伏前陆逆冲带是塔里木克拉通区与前陆区寻找大中型油气田的最有利地区。     

Palaeogene fossil <Emphasis Type="Italic">Populus</Emphasis> leaves from Lanzhou Basin and their palaeoclimatic significance

An angiosperm compression flora is found in Palaeogene from Lanzhou Basin and the cuticular analysis of Populus davidiana Dode in the flora is carefully made. Furthermore, the fossil cuticles are compared with the epidermal structures of extant Populus leaves growing in different environments, i.e. moist, semimoist, and semiarid to arid climatic regions. The present experiments indicate that mature leaves of P. davidiana show leaf size from big to small, leaf cuticles from thick to thin and anticlinal walls of epidermal cells from faintness to clarity along with the increase of lattudes of the plant distributions, the climatic variation from moist to arid, the annual precipitation from more to less and the annual mean temperature from high to low. The fossil P. davidiana differs from the specimens collected from Shandan in semiarid to arid climatic regions but closely resembles the Wushan leaves in a semi-moist climatic area in a lot of features. In a word, the new research may reflect that the flora lives in a semi-moist climatic environment. The present discovery of compression of Paleogene Populus davidiana is of great significance to studying vegetation types, climatic and environmental changes during the primal uplifting of the Qinghai-Tibet Plateau.     

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.     

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…     

青藏高原若尔盖盆地草地沙化成因分析及治理对策

根据野外调查与遥感解译,结合前人研究资料,论述了若尔盖盆地沙化草地分布特征,探讨了草地沙化日趋严重的原因,提出了对青藏高原生态研究、长江、黄河上游沙漠化的防治均具有重要意义的治理对策.     

太湖入湖河流水质指标的年变化规律

对位于太湖西部宜兴市大浦镇的一条入湖河流水质的年变化规律进行了分析.结果表明:(1)河道全年总氮含量监测值均劣于Ⅴ类水指标,其他水质指标相当于Ⅱ～Ⅳ类水水质,水体的富营养化主要体现为总氮含量的超标;(2)除TN、TP,其余水质指标在植物的生长季均劣于非生长季;(3)水体中BOD5、CODMn、Chla含量的变化主要受温度的影响,温度变化是水体有机质含量变化的触发因子;(4)降雨量与水体TP含量呈显著正相关,但对其他水质指标影响较小,说明水体生态过程对TP的影响相对较小,TN等指标更易受水体生态过程的影响.