造山型金矿容矿建造分类、成矿模式及找矿勘查

造山型金矿床指造山过程中形成的后生脉状金矿床,受构造、建造双重控制,是全球最重要的金矿勘查类型。按容矿岩石建造的不同,造山型金矿可分为绿岩带型（包括绿片岩型、BIF型和花岗- 片麻岩型3个亚类型）、浊积岩型、碳酸盐岩型和浅成侵入岩型,构成了造山型金矿床完整的成矿谱系。不同类型之间具有紧密的时空和成因联系,可互为找矿标志。绿岩组合和浊积岩系具有高的金丰度,既是容矿岩系,也是重要的矿源层,多类型造山作用驱动大规模区域性流体活动,造就了造山型金矿省/巨型成矿带,岩浆流体叠加和“热机效应”是形成超大型金矿床的重要因素。构建了多源区域性流体+岩浆流体叠加的地壳连续成矿模型和造山型金矿区域成矿模式,强调了多旋回造山作用对造山型金矿的成矿意义。“富金矿源层+剪切变形带+浅成侵入岩”组合是大型金矿系统的勘查选区标志,靶区优选的目标是获取找矿潜力大的优质矿权;矿权区勘查的优先目标是发现可规模化露天开采的矿床（体）,通过化探异常评价和浅钻追索次生富集带,可快速发现主矿体;矿区深部找矿（深度>300 m）潜力巨大,主攻目标是资源量大、品位高的热液通道相的厚板状或筒状矿体。     

铝片还原-硫酸铁铵容量法测定钛铁矿中高含量

试样经碱熔,盐酸提取的钛,在以盐酸、硫酸、磷酸组成的强酸性溶液体系中,利用铝片的强还原性,还原四价钛为三价钛。再用三价铁氧化三价钛为四价钛,过量的三价铁离子与硫氢酸根离子生成血红色络合物,根据此原理测定高含量钛。实验证明,溶液在此强酸性体系中,隔绝空气和控制时间的条件下,其含量范围在0.13%～100%内,测定结果准确度高。     

滇中富民县宝石洞旅游地质特征与成景机制探讨

滇中富民县宝石洞岩溶地下河洞穴景观系统规模适中,洞内岩溶景观千姿百态,洞中有宝(玛瑙),洞外有优美的生态环境和多元民族宗教文化以及潜在的温泉资源,加上优越的交通区位,旅游要素集群度较高,具较高开发价值.文章根据宝石洞地区区域地质背景,分析了该地区区域地史演化特征,根据本次对宝石洞的实地探测成果,总结了宝石洞旅游地质特征...     

世界主要海洋强国综合实力测评研究

文章在回顾世界海洋强国发展历程和分析现阶段发展特点的基础上,构建国家层面的海洋综合实力评价指标体系,并结合层次分析法和加权积决策理论建立了综合实力测评模型。通过选取世界上8个有代表意义的海洋强国,结合其海洋综合实力的现状分析,利用测评模型对其进行测评排序,为我国"海洋强国"战略的科学规划提供参考。     

海洋发光弧菌生长和发光条件的研究

海洋生物发光研究对渔业、环境监测等有着举足轻重的意义。根据从湛江东海岛海域沉积物样品中分离出的一株海洋发光弧菌(Vibrio sp.,编号为D2),对这株菌的生长和发光条件进行了初步研究。实验结果表明,海洋发光弧菌D2在pH7.0、温度35℃、NaCl浓度为2.0%时,生长状态最好;在pH5~6、温度20℃、NaCl浓度为3.0%、细菌密度OD600达0.08时,发光强度最高。     

长江-淮河流域短时暴雨洪涝灾害危险性预警评估及验证

洪涝灾害危险性预警分析是防灾减灾的重要基础,在灾害发生前进行预警,可以有效减轻灾害带来的影响。本文以2020年6—8月长江-淮河流域洪涝灾害为研究案例,首次利用前3天累计降水量(前期状态),当前时次土壤湿度(当前状态)和预测日降水量(未来状态)作为致灾因子,基于改进的层次分析法建立危险性预警分析模型。通过县域灾情信息验证表明,评估正确率达74.46%,遗漏率仅5.59%,评估结果与实际灾情吻合性好;同时对预警准确性和时相一致性进行评价,最大值(县内最高指数)的预警率达到81.6%;“特大型”暴雨洪涝灾害中的预警达到77.3%以上,且灾害在前3~5天危险性指数普遍提升,存在有效预警。本文方法对于长江—淮河流域短时暴雨洪涝灾害危险性预警有较好的准确性和可靠性,可提供防灾减灾决策依据。     

Formation and evolution of the modem warm current system in the East China Sea and the Yellow Sea since the last deglaciation

To reconstruct the formation and evolution process of the warm current system within the East China Sea (ECS) and the Yellow Sea (YS) since the last deglaciation, the paleoceangraphic records in core DGKS9603, core CSH1 and core YSDPI02, which were retrieved from the mainstream of the Kuroshio Current (KC), the edge of the modem Tsushima Warm Current (TWC) and muddy region under cold waters accreted with the Yellow Sea Warm Current (YSWC) respectively, were synthetically analyzed. The results indicate that the formation and evolution of the modem warm current system in the ECS and the YS has been accompanied by the development of the KC and impulse rising of the sea level since the last deglaciation. The influence of the KC on the Okinawa Trough had enhanced since 16 cal kyr BE and synchronously the modem TWC began to develop with the rising of sea level and finally formed at about 8.5 cal kyr BP. The KC had experienced two weakening process during the Heinrich event 1 and the Younger Drays event from 16 to 8.5 cal kyr BP. The period of 7-6 cal kyr BP was the strongest stage of the KC and the TWC since the last deglaciation. The YSWC has appeared at about 6.4 cal kyr BP. Thus,the warm current system of the ECS and the YS has ultimately formed. The weakness of the KC,indicated by the occurrence of Pulleniatina minimum event (PME) during the period from 5.3 to 2.8 cal kyr BE caused the main stream of the TWC to shift eastward to the Pacific Ocean around about 3 cal kyr BP. The process resulted in the intruding of continent shelf cold water mass with rich nutrients. Synchronously, the strength of the YSWC was relatively weak and the related cold water body was active at the early-mid stage of its appearance against the PME background, which resulted in the quick formation of muddy deposit system in the southeastern YS. The strength of the warm current system in the ECS and the YS has enhanced evidently, and approached to the modern condition gradually since 3 cal kyr BP.     

基于改进BP神经网络的海底底质分类

通过采用遗传算法优化神经网络初始权值的方法,将GA算法与BP神经网络有机结合,应用于海底底质分类。基于多波束测深系统获取的反向散射强度数据,应用改进的BP神经网络分类方法,实现对海底基岩、砾石、砂、细砂和泥等底质类型的快速、准确识别。通过实验比较,GA-BP神经网络分类精度明显高于BP神经网络,证明了该方法的有效性和可靠性。     

卫星导航系统定位精度评估

对用户等效距离误差结合精度衰减因子（DOP）值的精度评估方法进行了阐述,提出根据单站DOP和全球DOP进行系统定位精度评估的两种方法,仿真证明,两种方法评估结果相当。