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1993年9月10日,中国地质学会第35届理事会第4次常务理事会议讨论通过了中国地质学会第四届青年地质科技奖名单,决定授予黄润秋等9名同志中国地质学会第四届青年地质科技奖金锤奖和王剑等30名同志银锤奖。 第四届青年地质科技奖评选共推荐候选人65名,他们分别来自内蒙、新疆、辽宁、湖南、湖北、宁夏、 相似文献
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为表彰具有“献身、创新、求实、协作”的科学精神和科学道德及学风的40周岁以下的青年地质工作者，向中国地质学会成立百年献礼，学会于2022年2月22日启动了第十八届青年地质科技奖(金银锤奖)申报及推荐工作。近期，中国地质学会组织召开第十八届青年地质科技奖(金银锤奖)终评会议，评选产生了第十八届青年地质科技奖(金银锤奖)获奖者。会议决定授予梁前勇等10名同志“第十八届青年地质科技奖——金锤奖”荣誉称号，授予曹文庚等40名同志“第十八届青年地质科技奖——银锤奖”荣誉称号（获奖名单见附件）。 相似文献
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两年一次的中国地质学会青年地质科技奖评选工作日前结束,经中国地质学会第36届理事会第4次常务理事会议批准,授予高俊等10名同志金锤奖、于学峰等40名同志银锤奖。这次共有100名候选人申请,他们是各省级地质学会、各专业委员会和各理事单位在数以千计的候选人中推荐上来的。至此,中国地质学会青年地质科技奖已经评选6届,共有41人获金锤奖、158人获银锤奖。其中10位金锤奖获得者被推荐并荣获“中国青年科技奖”。 相似文献
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<正>2017年8月20日,中国地质学会召开第16届青年地质科技奖(金、银锤奖)终评会议,评选产生了第16届青年地质科技奖(金、银锤奖)获奖者。会议决定授予10位青年地质学家"第16届青年地质科技奖——金锤奖"荣誉称号,授予40位青年地质学家"第16届青年地质科技奖——银锤奖"荣誉称号(名单见后)。 相似文献
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正2019年9月21日,中国地质学会召开第十七届青年地质科技奖(金、银锤奖)终评会议,评选产生了第十七届青年地质科技奖(金、银锤奖)获奖者。会议决定授予李大鹏等10名同志"第十七届青年地质科技奖——金锤奖"荣誉称号,授予陈尚斌等40名同志"第十七届青年地质科技奖——银锤奖"荣誉称号(名单见后)。此次评审经申报、推荐、形式审查、初评、公示、终评等严格的评选程序,从我国地质行业各部门单位推荐的361名候选人 相似文献
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中国地质学会第八届青年地质科技奖评选工作已於2001年12月顺利完成。截止2001年12月1日,中国地质学会各理事单位、各专业委员会和各省级地质学会共推荐青年地质科技奖候选人117名,候选人工作单位遍布全国地质行业各部门。2001年12月14日-15日,中国地质学会组织以陈毓川院士为评审组组长的24名专家,对入围候选人进行了认真、细致地评 相似文献
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继中国科协1988年8月颁布首届“青年科技奖”以来,全国各条战线又涌现出一大批优秀青年科技工作者,经中国科协第二届青年科技奖评审委员会评选,101名青年科技工作者荣获第二届“青年科技奖”,其中有五名青年地质工作者.中国地质学会推荐了三名候选人,石彦民和董树文二位同志光荣入选.颁奖活动将在1991年5月召开的中国科协第四次全国代表大会期间举行. 相似文献
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试论地质勘查单位档案工作规范化管理 总被引：1，自引：0，他引：1
地勘单位的档案资源是地质工作历史的最真实的记录和珍贵的历史资料。它客观地反映了各个历史时期地质工作状况。本文主要论述了地勘单位档案规范化管理的重要性和必要性,探讨了档案规范化管理的组织建设和制度建设,对地质档案的开发和利用提供了可行的措施。 相似文献
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《International Geology Review》2012,54(7):843-845
The need for rapid storage and retrieval of geologic information is discussed briefly. The writer proposes to encode such information on perforated cards, from which it can be transferred to any other recording device. Hopefully, eventually, there will be an international arrangement where such information can be retrieved rapidly and used effectively anywhere in the world. Three examples are chosen to show how the proposed system works: A stratigraphic section, igneous phenomena, and tectonic deformations. These are set up in three tables representing the perforated cards and the proposed items are discussed in some detail. – E. Ingerson. 相似文献
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煤田地质勘探工作,过去多侧重于煤炭资源的勘探,对与矿井（含露天矿,以下同）设计、施工、生产有较大关系的工程地质工作有时重视不足,如精查报告中,对第四纪地质的章节阐述就极为简单,对勘探区域内（尤其是工业广场、工人村等建筑范围）的物理地质现象、地形地貌、岩土的物理力学性质和工程地质条件等所做的工作就更显不够,以致不能较好的指导设计、施工与生产。因此,在煤田地质勘探中做好工程地质工作,是当前一项紧迫的任务。 相似文献
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南岭构造带横跨扬子地块、江南造山带以及华夏地块,是中国钨锡铅锌铀等有色金属和铌钽锂铯与稀土等关键金属成矿带.通过综述近十五年来的研究进展,总结了南岭构造带基础地质特征与成矿地质背景.扬子与华夏地块沿永州-桂林-柳州一线于新元古代拼合,但缺乏直接的地质证据,需对龙胜蛇绿混杂岩和鹰扬关混杂岩进行深入研究.新元古代至中生代花岗岩二阶段模式年龄TDM2值揭示2.0~1.2 Ga为南岭构造带的主要地壳增生期.相似的花岗岩特征和构造线方向指示广西期和印支期造山机制均为陆内造山作用,是华南大陆南侧不同板块之间拼贴远程应力场的产物.燕山早期花岗岩εHf(t)值沿南岭构造带自西向东显著减小,而TDM2值明显增加,指示湘南-桂北-粤北地区在晚侏罗世经历了古太平洋板块断离和软流圈上涌并发育强烈的壳幔相互作用,为南岭构造带东段华夏地块上钨锡等多金属成矿提供了成矿物质来源和有利的伸展构造背景.南岭构造带西段扬子地块构造相对稳定且显生宙岩浆活动较弱,新元古代大塘坡组和寒武系底部页岩是良好的页岩气勘探目标.综合沉积、岩浆以及构造变形,华南中生代特提斯构造域向古太平洋构造域转换开始于晚三叠世. 相似文献
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正On 1–5 September 2014,the China Geological Survey Bureau held a 2015–2020 Geology and Mineral Resources Investigation and Assessment Special Planning and Deployment Meeting to plan the next six years in order to invest nearly ten billion US dollars to implement 9 programs and 50 projects with the aim of developing geological survey work,and to play a leading role in ensuring sustained and stable development.1 The Land Energy and Mines Geological Survey Program 相似文献
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《China Geology》2020,3(1):153-172
Serving as a way to understand the material composition, structure, and dynamic process of the Earth’s interior, deep earth exploration is driven by not only mankind’s pursuit of natural mysteries but also mankind’s basic need to obtain resources and guarantee economic and social development. The first phase of deep earth exploration of China (SinoProbe) was carried out from 2008 to 2016 and tremendous results were achieved. In 2016, the China Geological Survey launched a Deep Geological Survey Project (also referred to as the Project) to continuously explore the deep Earth. Focusing on the national energy resources strategy, the Belt and Road Initiative, and major basic issues of the geological survey, the Project was carried out in Songliao Basin (an important energy base in China) and major geological boundaries and tectonic units including Qilian Mountains-Tianshan Mountains and Qinzhou-Hangzhou juncture belt. The purpose of it is to reveal the process, structure, and forming patterns of the deep ore deposits and petroleum reservoirs, clarify the evolutionary pattem and controlling factors of Mesozoic environmental climate, and discover deep fine structures of key orogens, basins, and mountains by comprehensive geophysical exploration and scientific drilling. Great achievements have been obtained after more than three years of efforts, including a cumulative 1552 km of deep seismic reflection profiles and magnetotelluric profiles, an ultra-deep continental scientific drilling well, a scientific drilling pilot hole, and a magnetotelluric array and a portable broadband seismic array, both of which cover South China. Moreover, significant progress has been made in ultra-deep drilling technology, deep oil and gas discovery in Songliao Basin, and basic geological issues of Qilian Orogen and Qinzhou-Hangzhou juncture belt in South China, greatly accelerating the deep earth exploration in China and further consolidating China’s position as a power in deep earth exploration. 相似文献
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DENG Yiying CHEN Dongyang FAN Junxuan SHI Yukun HOU Xudong YANG Jiao XU Wenxiang 《《地质学报》英文版》2019,93(Z1):11-13
正1 Introduction Geological outcrops or sections are the basis of geological research.However,the traditional methods for presenting them are mainly photos which fall short of delivering a true visual sense (Deng et al.,2009;Hou et al.,2014).With the continuous development of image acquisition technology using single-lens reflex camera (SLR camera),image synthesis,large file storage and acquisition,panoramic visualization and network technology,high-resolution panorama as a means to display 相似文献
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Simulation of Geological Contacts from Interpreted Geological Model Using Multiple-Point Statistics 总被引：2，自引：1，他引：1
Alexandre Boucher Joao Felipe Costa Luis Gustavo Rasera Eduardo Motta 《Mathematical Geosciences》2014,46(5):561-572
Applications of multiple-point statistics (mps) algorithms to large non-repetitive geological objects such as those found in mining deposits are difficult because most mps algorithms rely on pattern repetition for simulation. In many cases, an interpreted geological model built from a computer-aided design system is readily available but suffers as a training image due to the lack of patterns repetitiveness. Porphyry copper deposits and iron ore formations are good examples of such mining deposits with non-repetitive patterns. This paper presents an algorithm called contactsim that focuses on reproducing the patterns of the contacts between geological types. The algorithm learns the shapes of the lithotype contacts as interpreted by the geologist, and simulates their patterns at a later stage. Defining a zone of uncertainty around the lithological contact is a critical step in contactsim, because it defines both the zones where the simulation is performed and where the algorithm should focus to learn the transitional patterns between lithotypes. A larger zone of uncertainty results in greater variation between realizations. The definition of the uncertainty zone must take into consideration the geological understanding of the deposit, and the reliability of the contact zones. The contactsim algorithm is demonstrated on an iron ore formation. 相似文献