钱塘江涌潮简析与预报

根据１９９１年观测资料，仑前潮位站出现涌潮１８４次，涌潮次数多少与江道地形变迁及上游下泄流量大小有关。涌潮高度在１．２－２．２ｍ之间，与涨潮潮差成正比。涌潮潮时预报方法有传播时间法和隔日滞后时间法。涌潮高度的预报，可根据当天涌潮高度预测后一天涌潮高度，也可根据下游站的涌潮高度预报上游站的涌潮高度。     

哈密盆地区域地貌的基本特征

本文对哈密盆地的现代地貌进行了成因分类，并系统地讨论了地貌结构特征，同时结合灾害地貌过程和资源特点提出了合理利用资源的几点意见。     

论黄河上游多民族经济开发区资源开发战略

本文在分析黄河上游多民族经济开发区资源特点的基础上，论证了经济区资源开发模式及开发战略，并就经济蛆内各区域非平衡开发及开发时序提出了一些见解。     

天山头屯河水沙情势变化分析

近三十年水文、气象资料表明，头屯河水量的９０％由制材厂水文站以上流域汇入，河道泥沙主要来自水库实验以上中游河段，河道来水量与输沙量变化不完全一致，年径流量的多寡与年降水量密切相关，河流输沙量则与春、夏季节的暴雨或阵发性降水有关。头屯河最大月径流量出现在７月份，而最大月输沙量则出现在６月份，与最大降水月（６月）出现时间一致。汛期河道来水量占全年总数的６０－６５％，而来沙量占全年总数的８０－８５％，后     

博斯腾湖流域气候及湖陆风

通过流域多个气象站的资料，分析了流域气候条件，并通过对湖区测点的气象观测资料与陆区测点－ 焉耆站的同步资料对比分析，讨论了博斯腾湖区域小气候其湖陆风特征。     

Magnetostratigraphy of the Red Beds in the Hengyang Basin

Abstract This paper discusses the Cretaceous-Tertiary magnetic polarity sequence of the the Hengyang Basin on the basis of magnetostratigraphic study. The age of each stratigraphic unit has been determined with the magnetic polarity time scale combined with ³⁹Ar/⁴⁰Ar dating, thus providing evidence for determining the geological ages of different formations. The authors assign the age of the Dongjing Formation of the Hengyang Basin to Early Cretaceous, the Shenhuangshan Formation to Early-Late Cretaceous, the Daijiaping Formation to Late Cretaceous, and the Dongtang and Xialiushi formations to Palaeocene.     

Trona resources in southwest Wyoming

Bedded trona (Na₂CO₃·NaHCO₃·2H₂O) in the lacustrine Green River Formation of Eocene age in the Green River Basin, southwest Wyoming, constitutes the largest known resource of natural sodium carbonate in the world. In this study, 116 gigatons (Gt) of trona ore are estimated to be present in 22 beds, ranging from 1.2 to 11 meters (m) in thickness. Of this total, 69 Gt of trona ore are estimated to be in beds containing less than 2 percent halite and 47 Gt in beds containing 2 or more percent halite. These 22 beds underlie areas of about 130 to more than 2,000 km² at depths ranging from about 200 m to more than 900 m below the surface. The total resource of trona ore in the basin for which drilling information is available is estimated to be about 135 Gt.Underveloped trona beds in the deeper southern part of the basin may be best developed by solution mining. Additional unevaluated sodium carbonate resources are present in disseminated shortite (Na₂CO₃·2CaCO₃) in strata interbedded with the trona and in shallow sodium carbonate brines in the northeast part of the basin. Estimates of the shortite and brine resources were not made.     

50年代以来黄河下游河道的萎缩及其原因*

根据黄河下游7个控制断面的深泓高程、平均河底高程、滩槽高差及过水断面面积的历年变化,可以看出黄河下游河道的萎缩过程,大型水利工程的运用及引黄灌溉加速了下游河道的淤积和萎缩。     

烃类微渗漏的地物波谱探测原理与方法研究

通过对新疆塔里木盆地北缘油气谱的实测和分析，结合烃类微渗漏理论，讨论油气信息的波谱特征和遥感直接探测的机理。运用遥感技术探测油气信息，一是探测烃类微渗漏产生的地表理化异常，二是直接探测渗漏运移到地表的烃类物质或土壤吸烃信息。在塔北试验区，烃类组分异常是最直接，最有意义的标志，２．３２－２．３６μｍ的烃类吸收双谷位置，被确定为塔北地区油气遥感探测波段。