祁连山东段冲积扇的发育时代及其成因

第四纪期间祁连山东段山麓地带广泛发育了多级冲积扇,它们是研究区域构造抬升与气候变化最为直接的载体.本文主要通过ESR,IRSL以及14C等绝对测年手段对该区冲积扇的形成年代进行研究,结果表明祁连山东段北麓最高级冲积扇形成于0.85 MaBP,而毛毛山南麓的最高级冲积扇形成于0.43 MaBP.随后各地又相继发育了0.25,0.16,0.06,0.01 MaBP等多级冲洪积台地.根据主要冲积扇的形成年代及其与区域构造气候事件的对比,认为它们是构造运动与气候变化共同作用的产物.     

民族精神与浙东史学

浙东史学是指在一定的区域范围内，先后传承，有着相近的治史宗旨或方法的史学流派。它从南宋时期开始形成，经过元明、清初，一直到晚清，其发展不绝如缕。并在其发展的过程中，形成了独有的特色，其中民族精神是其显著特色之一。     

湖北七姊妹山自然保护区兽类资源初步研究

对七姊妹山自然保护区的兽类资源进行了考察，报道兽类共58种，隶属于8目22科，保护区有国家重点保护兽类42种：Ⅰ级3种，Ⅱ级12种，有益的或有重要经济、科研价值的兽类27种；有CITES附录的兽类21种，对兽类的区系组成、种群数量和保护现状进行了研究，并提出了保护对策。     

农田蒸散和干旱的计算及其分析

农田蒸散是形成土壤干旱的主要因素。本文采用陶祖文的彭曼修正公式对冀东地区的唐山、秦皇岛、乐亭、遵化等地3～11月的可能蒸散与可能实际蒸散进行了计算,并与本省南部的曲周做了可能蒸散量的对比分析。在统计分析的基础上,按《干旱分析方法的探讨》一文给出的华北地区干旱指标,用唐山农业气象站1980～1989年观测旱作地段的土壤湿度资料,对当地干旱的发生与干旱的指标进行了分析和验证。     

龙门山中北段重磁场特征与深部构造的关系

利用平均重力场与深部地壳测深资料估算了龙门山及邻区莫霍面的深度变化,表明龙门山地区正处于莫霍面由东南向西北的陡降带上。均衡重力异常计算结果显示该区为正异常。对航磁异常的向上延拓反映出茂汶杂岩体是“无根”的。此外还应用角度平均径向能谱法反演了该区深部磁性基岩的顶面与底面深度。结果表明,龙门山地区上地壳是由若干块体拼合而成的,川西拗陷带内的磁性界面呈现出向龙门山地腹下插的格局。     

The discovery of early Permian reef belt in east Kunlun and its significance

The early permian reef belt is distributed in the southern side of eastern Kunlun, north area of Qinghai-Tibet Plateau. The core-reef facies of thc reel extends from Tuosuo Lake to Huashixia. Lots of reef breccia was found at the southern slope of the mre-reef belt, and to the north of the reef belt there is back-reef limestone. Cacisponges, hydrozoa, bryozoa,Tabulozoa, Tubiphytes and red algae are the main frame-building organisms.Archaeolithoporella, laminated blue-green algaes,Tabulozoa andTubiphytes played a role of binding or encrustating. There are many kinds of epibiont in the mf, including brachiopod, gasterid, foraminifera, echinoderm and simple coral. The type and the characteristics of the reef-building organisms in eastern Kunlun and Animaqing are basically thr same as those in the south of Chi     

Discovery and character of the Kunlun-Yellow River Movement

Based on geomorphological, tectonic and sedimentary data, a Kunlun Yellow River Tectonic Movement has been recognized in 1 10-0 60 Ma B.P. This tectonic movement, which leads to uplift of the Qinghai_Xizang (Tibet) Plateau from 1 500 to 3 000-3 500 m, is periodic, abrupt and changeable in the movement rate of uplifting and slide slipping.     

Carbon isotope anomaly in marbles associated with eclogites from the Dabie Mountains

This is a report of carbon isotope anomaly in marbles associated with the UHP eclogites from the Dabie Mountains. The results place constraints on the degree of crust-mantle interaction during the UHP metamorphism.     

Isotope composition of helium in eclogite from the Dabie Mountains, central China and its geological significance

Isotopic geochemical characteristics of helium in garnet and omphacite of eclogite in the Dabie Mountains are discussed. Concentrations of 3He and 4He in garnet and omphacite are 3.9×10 -14- 24.0×10 -14 and 0.48×10 -7-9.42×10 -7cm+3·g -1, respectively. Values of 3He/ 4He have a range of (1.19-4.63)×10 -7. Helium in the eclogite is derived from both mantle and crust. Isotopic geochemical data of helium indicate that eclogite in the Dabie Mountains might be formed in depleted mantle and the age of the cologite would be Indo-China epoch.