C.I.P.W标准矿物计算方法的PC—1500袖珍计算机BASIC语言程序

C.I.P.W标准矿物计算是火成岩岩石学研究中常做的工作。倘若手算,耗时费力,且难保一次性计算结果无误。为此,针对12种氧化物设计的,上机运行通过的BASIC语言程序可以换算20种基本标准矿物,适用于碱性、酸性、中性、基性和超基性岩类中火山岩及侵入岩的数十个岩石种属。计算和输出,一件样品约一分钟即可完成,且精度颇高。计算结果采用格式化输出,清晰醒目,易于查阅和使用。     

PALEOGEOGRAPHY OF THE SEYCHELLES BANKAND THE NORTHWEST MADAGASCAR SHELFDURING THE LAST GLACIO EUSTATICREGRESSION (18,000 a B.P)

The-Seychelles Bank and Madagascar Shelf in the western Indian Ocean were explored geologically during a cruise of the R/V "professor Shtokman" in 1986. Using the data of relief, sediment characteristics and their sequences of strata, paleogeographic maps (18,000 a B.P.) of these areas were produced. These maps show that the Bank and the Shelf are carbonate platforms with complicated topography. The data indicate an important role of sea level oscillation in relief development of this area.     

Genetic variation in parthenogeneticArtemia from the Shandong Peninsula,P.R.C.

Results are presented of a survey of isozyme frequencies in parthenogeneticArtimia from six salterns in the Shandong Peninsula, P.R.C. Three of the eleven enzymes we scored using polyacryamide gel electrophoresis proved to be useful for analysis of electromorph frequency variation. These enzymes are tetrazolium oxidase (TO), lactate dehydrogenase (LDH), and malate dehydrogenase (MDH). Each of these systems showed extensive isozyme variation both within and between salterns. In addition, we have examined the possibility that electromorph frequencies may vary as the result of natural selection for adaptation to specific salinity, or salinity-associated environmental conditions. An indication of clinal variation was found in two series of ponds differing in salinity, however more extensive data are needed before it is possible to conclude that these patterns are the result of natural selection. Finally, the use of isozyme analyses such as ours, for unraveling taxonomic problems inArtemia is discussed.     

Comparative studies on the larval development of the penaeid shrimps,Penaeus Chinensis,P. merguiensis andP. penicillatus

The morphology of larval and 1st postlarval stages ofPenaeus penicillatus are described. Results from comparative studies on larval development ofP. penicillatus, P. merguiensis andP. chinensis are as follows: These three species could not be identified during their naupliar stages. In the 1st protozoea, the antennule L1/L2 value is 1.7–2.0 inP. merguiensis, but less than 1.7 inP. chinensis andP. penicillatus; in the 2nd protozoea, the supra-orbital spine inP. chinensis is not bifurcated, while those ofP. merguiensis andP. penicillatus are bifurcated; in the 3rd protozoea, there is a minute (or no) dorso-median spine on the posterior margin of the 1st and 2nd abdominal somite inP. chinensis, but they are prominent inP. merguiensis andP. penicillatus. In the mysis and 1st postlarval stages,P. chinensis differs fromP. merguiensis andP. penicillatus in having 9 (8 in the other 2 species) long setae on the exopod of pereopods 1–3; additionally, one dorsal tooth appears on the rostrum ofP. chinensis in the 2nd mysis and that of the other 2 species in the 3rd mysis;P. chinensis has 2 (mostly) or 1 dorsal tooth on the rostrum in the 3rd mysis and 2–3 in the 1st postlarva, whileP. penicillatus andP. merguiensis have only 1 in the 3rd mysis and 1st postlarva. Comparative studies on larval development showedP. penicillatus has closer affinity withP. merguiensis than withP. chinensis. Contribution No. 2218 from the Institute of Oceanology, Chinese Academy of Sciences     

DIETARY MANGANESE REQUIREMENT OF P. VANNAMEI

M0DUonONManganeseisanessentialelernentfororganismss.TherearernanypublishedreportS0ntheMnrequdritSoritSdrionfishes,indudingrainb0wtrout,channelcatfish,Atianticsalmon,cornmncarp,grasscarp,tilapia,Ctc.Kanamwaetal.(l984)andLiCtal.(l992)reportedtheresultSoftheiraseawhonthernanganeserequdritSofjuvenileP.japonicusandP.chinensiS.Davisandhawrence(l99O)studndthetheofdietaryman-ganeseonP.vannameibydeletionofMnfromthendneralpedinasdri9udrieddiet.ThepresentstudyontheefhaofgtadedleveIs0frnanganeses…     

A comparison of the bacterial microflora between coastal sites in Qingdao, P. R. China and Loch Fyne, Scotland

Aerobic, heterotrophic bacteria, recovered from two sites located on the west coast of Scotland, were compared to cultures obtained in a similar way from industrial, aquacultural and clean sites in the vicinity of Qingdao, Shandong, P. R. China. Gram-negative bacterial cultures were examined by BIOLOG-GN, and the data analysed by the simple matching (S_SM) and Jaccard coefficients (S_J) and unweighted average linkage clustering using NTSys. The output revealed that 20% of the bacteria, namely, Acinetobacter johnsonii, Aquaspirillum dispar, Pseudomonas spp. (two groups), Sphingobacterium sp., Vibrio, sp., V. campbellii, V. mimicus and V. hollisae, were common between the two geographical locations. However, the study revealed shortcomings with the BIOLOG-GN system for the study of coastal Gram-negative bacteria.     

《中华人民共和国国家自然地图集》问世——20世纪中国地球科学调查研究成果的系统汇编

《中华人民共和国国家自然地图集》是代表国家水平的一部大型综合性科学参考地图集,包括序图、自然环境、自然资源、自然灾害、自然利用与保护等五个部分18个图组,共540幅地图,115个图表与照片,以及近30万字的地图说明。图集为四开本共283页,中、英文版同时出版发行。这是20世纪中国地球科学的一项重大成果。     

STUDIES ON IMMUNODIAGNOSIS OFHEPATOPANCREATIC PARVO- LIKEVIRUS DISEASE OF THE CHINESEPENAEID, PENAEUS CHINENSISI. PURIFICATION OF THE VIRUS

The viral disease of penaeids is indistinct but highly dangerous because their symptoms are often masked by some secondary ones.In order to gain knowledge on how to prevent the occurrence and spread of this viral disease, diagnostic studies on the early phase of the hepatopancreatic parvo-like viral (HPV)disease of cultured Penaeus chinensis was conducted using immuno-serological techniques. The purification of HPV was successfully done by density gradient ultracentrifugation of cane sugar.     

Applicability of Perinereis aibuhitensis Grube for Fish Waste Removal from Fish Cages in Sanggou Bay,P.R.China

The present study investigated the applicability of integrated polychaete-fish culture for fish waste removal to offset negative impact induced by organic benthic enrichment.A field study demonstrated that deposition rate was significantly higher underneath the fish farm than that in control area.The material settling under the farm was characterized by a high amount of fish feces(45%) and uneaten feed(27%).Both feeding rate(FR) and apparent digestibility rate(ADR) increased with decreasing body weight,as was indicated by significantly a higher rate observed for the groups containing smaller individuals in a lab study.The nutrient in fresh deposited material(De) was higher than that in sediments collected under the farm(Se),resulting in lower feces production but higher apparent digestibility rate for the De group as feeding rate was similar.Consequently,higher nutrient removal efficiency was observed in the De group.A mass balance approach indicated that approximately 400–500 individuals m~(-2) is required for removing all waste materials deposited underneath the fish farm,whereas abundance can be lower(about 300–350 individuals m~(-2)) when only the fish waste needs to be removed.The results showed that a significant amount of waste had been accumulated in the fish cages in Sanggou Bay.The integration of fish with P.aibuhitensis seems promising for preventing organic pollution in the sediment and therefore is an effective strategy for mitigating negative effect of fish farms.Thus such integration can become a new IMTA(integrated multi-trophic aquaculture) model in Sanggou Bay.     

甘南毕家山铅锌矿床地质特征与成因

该矿床由两种类型矿化组成:(1)与所谓“微石英岩”密切共生的成层碎屑矿;(2)层状矿下伏石灰岩顶部的网脉矿。矿石硫化物在同位素组成上与围岩中的黄铁矿显然不同,其δ~(34)S值( 15至 18)表明可能是海水来源的,由海水硫酸离子在较高温度下无机还原而成。矿石中的碳酸盐矿物以较低的δ~(13)C和较高的δ~(18)O值不同于围岩石灰岩,前者表明可能有深成碳参加,后者表明成矿流体可能在较高温度下与硅酸盐岩石达到了同位素平衡。氧化硅的δ~(18)O值很重,落入海相燧石的变化范围。区域内没有火山活动的确切证据,以海水来源为主的成矿流体可能是沿分开不同地层小区的区域性断裂循环并被加热的。     

碧口地区复理石岩系特征及其构造环境

碧口地区晚元古代复理石岩系位于扬子板块西北缘,其主体由下部火山质碎屑浊积岩和上部陆源碎屑浊积岩组成。本文研究了复理石岩系中杂砂岩的岩石学、碎屑模型和岩石化学特征,并与不同板块构造背景下沉积的古代杂砂岩和现代深海砂成分进行了类比。研究表明,复理石岩系形成于沟弧盆系活动大陆边缘构造环境,杂砂岩属大陆岛弧型,物源区为活动大陆边缘的火山—深成岩浆岛弧造山带,源岩为钙碱性长英质火山岩及同源深成侵入岩,沉积盆地为岛弧及俯冲杂岩外侧的古海沟环境。     

宜阳地区罗圈组水下岸坡冲积扇的沉积特征

罗圈组作为冰川沉积物,已为地学界所重视。作者从地层层序、粒组分析和沉积环境等沉积学角度分析,初步认为它不管是冰川沉积物或是冰川—重力流改造沉积物,均应属水下岸坡冲积扇的沉积物。     

青海湖近8000年来演变及发展趋势

本文依据紫果云杉(Picea purpurea Mast)残木、部分地层测年资料、湖成地貌,结合树木年轮和湖水观测资料,探讨近8000年来青海湖演变史并概略预测其发展趋势:8000—3500a.B.P.为暖湿期,3500a.B.P.以来渐趋冷干—干旱,600a.B.P.以来又几经暖湿—冷干的更替;在不考虑温室效应的前提下,大致在133年后湖水达补耗水量平衡期;在温室效应的影响下,湖水将提前于下世纪中叶进入补耗平衡期。     

山东胶北隆起区荆山群

一、胶北隆起区变质地层划分沿革胶北隆起区前寒武纪变质地层广泛发育,很多地质工作者,曾在这里进行过研究工作。1958—1962年长春地质学院师生在该区进行一比二十万区域地质调查,首次将该区变质地层命名为“胶东群”,并自下而上划分为化山、旌旗山两个组,积累了大量的地质资料,从而为该区地质普查工作奠定了基础。 1968年,省局八○五队通过对该区一比二十万区调的修测,将该区(桃村断裂以西,沂沭断裂以东)胶东群自下而上划分为蓬夼、民山、富阳三个岩组,并将招平断裂以东,     

镇安二台子金矿控矿规律研究与盲矿体预测

在总结二台子金矿成矿规律的基础上,采用信息量和特征分析方法对矿区及外围进行了综合预测.之后,运用地球化学与构造应力分析相结合方法,对已知矿体进行了深部预测并定位.     

渭河盆地地貌特征水系格局与新构造活动

根据对渭河盆地地貌、水系格局的分析,本文提出:(1)渭河盆地地区新构造运动主要表现为以近东西向、北西向和北东向几组断裂控制下的断块运动;(2)断块运动自南而北呈波浪式发展,且具多期活动的特点,可分为老第三纪、中新世、上新世—更新世初、更新世末—全新等世四个活动期;(3)新构造运动具有明显南强北弱、东强西弱的差异性,华阴—华县一带最强,为应力集中区;(4)盆地新构造应力场的主压应力方向为48°～79°。     

南方涛动、热带海温与西北太平洋副高的联系

本文应用统计方法,首先探讨南方涛动指数与西北太平洋副热带高压的联系,然后分析赤道和热带太平洋区域海温对南方涛动的响应情况,同时分析南方涛动响应区域的海温与当时及滞后的西北太平洋副热带高压的联系,从中探讨南方涛动、厄尔尼诺海温异常及西北太平洋副热带高压之间的一种可能的相互作用机制。     

陕西蓝田红门寺地区丹凤群构造变形特征

本文对蓝田红门寺地区丹凤群的变形特征,提出至少经历过三期主要构造变形及混合岩化作用。     

CSCO_3 CYCLES IN SALAWUSU RIVER BASINSINCE 150KA B.P.

About 70years ago，Frenc卜卜alaeohdoglst回LL sc卜dars al卜ome and a卜road卜ave successively con－HARD de Chardin P．et al．Initiated the Quaternary ducted large amount ofwork on the Later Quaternarygeologlcal research In the ＞alawusu River Basin of strata（TEILHARD，1924； YUAN，1978； LI，1987；desert region of Northern China and established th，ZHENG，1989； SUN et al，1996； LI et al，1993），Salawusu Formation门EILHARD，1924）．Sine，then，palaeobiology…     

运城盐湖盐类矿床特征及其成因探讨

分析了运城盐湖盐类矿床的地质特征,指出其剖面上的周期性、平面上的迁移性,演化过程的波浪性,构造环境的峰谷性,成矿物质的多源性,据此提出盆－岭式成盐新模式。