实际晶体形态计算机绘图   总被引：1，自引：0，他引：1  

周芬娜  王文魁 《地球科学》1992,17(2):159-169

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黄山第四纪泥砾沉积物的成因分析   总被引：8，自引：1，他引：8  

周秉根  李刚 《冰川冻土》1992,14(4):360-365

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中国东南沿海及邻近海区一种独特的大陆增生方式——转换断层向俯冲体系的转变     

周祖翼 《上海国土资源》1992,(1)

闽东沿海构造带—东海陆架西缘断裂、钓鱼岛隆起带(台湾—宍道褶皱带)以及帛琉—九州洋脊在中生代期间先后经历了自转换断层向俯冲系统的转变,这种转变构成了中国东南及毗邻海区独特的大陆增生方式,它表明特提斯和古太平洋的演化对这一地区的中、新生代构造格局起着重要的制约作用。  相似文献   

新疆吉木乃县塔斯特金矿成因探讨   总被引：2，自引：1，他引：2  

董永观  邹永兴  王敬东  孔庆寿 《新疆地质》1992,(2)

塔斯特金矿床为一破碎带蚀变岩型金矿。通过稳定同位素、包裹体、成矿元素及成矿物理化学条件的研究,提出该矿的成矿溶液是岩浆水和大气降水之混合物。成矿元素主要来自深源侵入的二长花岗岩。成矿温度为中偏高温。成矿溶液为高盐度、高密度和高挥发份条件。为深源岩浆侵入的花岗岩中破碎蚀变岩型金矿。  相似文献   

矿石源标定射气仪的应用研究     

周永安  唐忠慧 《铀矿地质》1992,8(1):42-47

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赣东北元古代蛇绿岩Sm—Nd同位素年龄及地质意义   总被引：9，自引：0，他引：9  

邢凤鸣  徐祥  陈江峰  周禧泰  K.Afoland 《岩石矿物学杂志》1992,11(2):120-124

江南古陆东南缘赣东北弋阳—德兴—婺源一线有一条蛇绿岩带,普遍认为它是二个一级大地构造单元的分界线,形成于元古代。推断蛇绿混杂岩是元古代古洋壳俯冲时被挤上来的碎片;也有人认为它是中生代二大古陆之间的缝合线。Sm-Nd矿物等时线给出1034±16Ma(MSWD=1.0)的同位素年龄,它符合元古代缝合带的观点,而不利于中生代缝合带。  相似文献   

Chromite deposits in China and their origin   总被引：4，自引：0，他引：4  

Mei-Fu Zhou  Wen-Ji Bai 《Mineralium Deposita》1992,27(3):192-199

The major chromite resources of China occur in ophiolites and continental intrusions. Podiform chromite deposits are mainly developed in the Palaeozoic and Mesozoic ophiolitic mantle sequences. They occur as tabular, lenticular, or irregular masses hosted by dunite lithologies, or dunite lenses, or harzburgite associated with dunite lenses. Main stratiform deposits occur within the Archean Northern China craton and are named as the Gaosi-type deposits, which are contained in intrusions similar to their Alaskan-type counterparts and are characterised by their ring-shaped ores. Stratiform deposits are also found in Phanerozoic ophiolites. Chromites in the ophiolites are chemically divided into high-A1 and high-Cr types, both of which plot in the alpine type field. Chromites from the Gaosi-type deposits belong to high-Fe type, possessing uniform Al contents. The podiform chromitites were generated from magmatic pockets in the mantle sequences, whereas those deposits (such as the Dadao deposit) in cumulate sequences had a similar origin but crystallized at shallower depths. Stratiform Gaosi-type deposits should have formed by accumulation of chromites which were in equilibrium with an ultramafic magma with a uniform Al content.  相似文献   

The stability of merwinite in the system CaO-MgO-SiO2-H2O-CO2 with CO2-poor fluids     

Jincheng Zhou  L. C. Hsu 《Contributions to Mineralogy and Petrology》1992,112(2-3):385-392

The stability of merwinite (Mw) and its equivalent assemblages, akermanite (Ak)+calcite (Cc), diopside (Di)+calcite, and wollastonite (Wo)+monticellite (Mc)+calcite was determined at T=500–900° C and P _f=0.5–2.0 kbar under H₂O–CO₂ fluid conditions with X _{CO 2}=0.5, 0.1, 0.05, and 0.02. Merwinite is stable at P _f=0.5 kbar with T>700° C and X _{CO 2}<0.1. At P _f=2.0 kbar, the assemblage Di+Cc replaces merwinite at all T and X _{CO 2} conditions. At intermediate P _f=1 kbar, the assemblage Ak+Cc is stable above 707° C and Wo+Mc+Cc is stable below 707° C. The univariant curve for the reaction Di+Cc=Wo+Mc+CO₂ is almost parallel to the T axis and shifts to low P _f with increasing X _{CO 2}, with the assemblage Di+Cc on the high-P _f side. The implications of the experimental results in regard to contact metamorphism of limestone are discussed using the aureole at Crestmore, California as an example.  相似文献   

自回归总径流线性响应模型在洪水预报中的应用   总被引：1，自引：0，他引：1       下载免费PDF全文

李蝶娟  周冰清 《水科学进展》1992,3(2):142-148

采用自回归总径流线性响应(ATLR)模型建立淮河王家坝站洪水预报方案和海河流域南运河水系洪水预报调度方案.自回归TLR模型与TLR模型加误差自回归实时校正模型的结构相同,但前者计算简捷,预报精度也有所提高.  相似文献   

地理专家系统的试验研究   总被引：18，自引：0，他引：18  

马蔼乃  周长发 《地理学报》1992,47(3):252-259

80年代人工智能与地理学的结合产生了地理专家系统(GES)。地理专家系统是继地理信息系统之后,对地理知识与推理形式化,建立的具有一定地理专业水平的计算机软件系统。地理专家系统由地理数据库,地理知识库和地理推理机三大部分组成。地理数据库是GES的数据管理模块,我们设计了一套地理信息系统MCGIS来作为微机地理专家系统MCGES的综合数据库;地理知识库是GES的知识管理模块;地理推理机则是GES的推理控制策略的程序体现。本文结合一个用C语言自行设计的基于规则的产生式微机地理专家系统MCGES阐述了地理专家系统的原理和方法。  相似文献