GEOLOGICAL CHARACTERISTICS AND ORE

Being a part of Jiaoliao anteclise,Jiaodong peninsula comprises from north to so uth three second－order tectonic units,namely Jiaobei uplift,Jiaolai (depression ) basin and Jiaonan uplift.In the past,a number of economic gold deposits were d iscovered in Jiaobei uplift,which can be roughly classified into altered rock ty pe in the shattered zone (Jiaojia type) and quartz vein type (Linglong type).In recent years,the authors discovered Pengjiakuang gold deposit and Fayunkuang gol d deposit on the northeastern margin of Jiaolai basin.The Pengjiakuang gold depo sit occurs in epi－basin faults with decollement segregation character on the ma rgin of Jiaolai basin,and the orebodies are consistent with faults in attitude a nd distributed discontinously along faults in lenticular forms.Individual orebod ies are 300～400 m in length,0.39～19.45 m in thickness,and have gold grade of 1.0～26.8 g/t;native gold is disseminated in silicified,phyllic or carbonatize d tectonic breccia,with proved gold reserves as high as 20 t.The Fayunkuang gold deposit occurs in conglomerate of Early Cretaceous Laiyang Group on the margin of Jiaolai basin,and the host rocks have been extensively subjected to silicific a tion,pyritization,sericitization,carbonatization and chloritization.Orebodies st ratoid in form occur gently (dip angle 10° or so) along interlayers of conglome rate.Individual orebodies have maximum length of 400 m,oblique extension of 600～ 700 m and gold grade of 1.0～15.3 g/t,with gold reserves 12 t.Mining practice r eveals that gold－rich pockets are also controlled by several bed－cutting fault s of different attitudes.     

不同类型沉积物中脂肪酸的分布、演化和生烃意义

对近代海洋沉积物、泥炭、福山凹陷第三系泥岩、茂名盆地第三系油页岩和辽河盆地东部凹陷第三系沉积岩剖面等样品中脂肪酸类型和分布特征进行了分析与研究。结果表明以低等浮游动植物为主的沉积中，二元肪酸丰度相对比一元酸占优势。随深程度增加，沥青中脂肪酸高碳数相对减少，低碳数相对增高，偶碳估势逐渐消失。在辽河盆地东部凹陷埋深２２６６ｍ的泥岩中发现脂肪酸仍具有偶碳优势，证明沉积有机质中偶碳脂肪酸优势可以保存到生油高峰前的较高演化阶段，对低熟原油烷烃的生成和具奇碳优势有重要意义。     

基于1:100万土壤空间数据库的有机碳储量估算研究——以中国东北三省为例

以最近建成的中国1:100万土壤空间数据库以及《中国土种志》和省级土种志的土壤属性为基础,共收集东北三省736个土壤剖面理化分析数据,估算出该地区土壤有机碳总储量,并分析讨论了土壤有机碳密度在空间上的分布特征。结果表明,东北三省土壤有机碳密度平均为16.13 kg/m²,在空间分布上的总趋势为东北部高,西南部低,密度较高的有机碳主要分布在原始森林、湿地及部分农业耕作区中。土壤有机碳密度最高的土类为泥炭土和沼泽土等土类,最低的为石质土、风沙土等土类。     

不同光强下长茎葡萄蕨藻(Caulerpa lentillifera)直立枝和匍匐枝的光生理特征及其对升温的响应

海洋绿藻长茎葡萄蕨藻(Caulerpa lentillifera,又名海葡萄)因具有较高经济和生态价值而备受关注,光照和温度变化均会改变长茎葡萄蕨藻生理代谢,最终影响其经济价值和生态功能。文章比较研究不同生长光强下(40、80、120和160μmol·photons·m^–2·s^–1)长茎葡萄蕨藻不同部位,即直立枝和匍匐枝的生理和生化特征,以及其对升温(+3℃、+6℃和+9℃)的响应。结果显示,光强由40升至120μmol·photons·m^–2·s^–1时对长茎葡萄蕨藻相对生长率(RGR)的影响不显著,但是光强升至160μmol·photons·m^–2·s^–1时可使RGR降低49%。弱光下(40μmol·photons·m^–2·s^–1)直立枝的叶绿素(Chl a)和类胡萝卜素(Car)含量为匍匐枝的1.52和1.49倍;直立枝的Chla和Car含量随生长光强升高而降低,匍匐枝随光强升高而升高,二者蛋白含量则均随光强...     

POI数据在中国城市研究中的应用

兴趣点(Point of Interest,POI)数据的兴起带动了城市研究的革新.为梳理中国POI数据在城市研究的应用进展,阶段性总结其应用方向、数据分析方法及尚存不足,并为未来POI数据在中国城市发展中的应用提供思路和借鉴.应用CiteSpace工具对中国知网2010-2019年625篇相关文献进行知识图谱分析,结...     

新疆甘肃交界红柳河蛇绿岩中伸展构造与古洋盆演化过程

红柳河蛇绿岩中保存了大量伸展特征构造，如堆晶辉长岩层中发育丰富的辉长质糜棱面理、伸展褶劈理、小型韧性低角度正断层、韧-脆性共轭正断层和脆性正断层等伸展变形构造。蛇绿岩中伸展变形构造经历了完整的变形序列：从韧性变形、经韧脆性变形到脆性变形。构造几何学关系表明这些构造形成于红柳河古洋盆闭合之前洋壳扩张过程中。^40Ar／^39Ar年代学的研究确定了红柳河古洋盆演化的过程：洋盆扩张发育在462Ma之前，并在412Ma前闭合。     

五龙沟金矿区域地球化学异常特征及找矿标志

本文以地质及区域地球化学资料为基础，通过对五龙沟金矿区域地质—地球化学异常特征和找矿标志的研究；建立了该矿床的区域地球化学异常模型及找矿标志。对已取得的大量1：20万区域化探异常的筛选和评价，以及进一步提高金矿化探普查效果，均具有一定的积极意义。     

基于CMIP6强迫模拟分析人为气溶胶的气候效应(二)——诊断方法在分类评估中的重要性

对气溶胶气候效应开展分类评估并探讨诊断方法的合理性。人为气溶胶辐射效应对计算云辐射强迫的影响为0.38 W·m~(-2)。诊断评估气溶胶对云辐射强迫的影响需要排除这个偏差。两种基于不同试验设计诊断得出的半直接效应分别为0.21和0.09 W·m~(-2),存在显著差异。主要原因可能是人为气溶胶影响云辐射强迫的不同机制之间在模式模拟过程中不断地相互交织,不是简单的线性叠加关系。模式诊断得出的Twomey效应不仅包括Twomey效应本身,还包括Twomey效应引起的部分快速调整。总之,利用模式评估分析人为气溶胶气候效应需要注意审查试验设计和诊断方法的合理性。     

基于探地雷达的植物根系探测研究进展

植物根系在植物的生长发育、生态系统功能以及碳循环过程中具有重要作用,需要了解根系的直径大小、生物量、空间分布和三维构造等参数.传统的植物根系的探测方法具有破坏性,费时费力,而探地雷达(Ground Penetrating Radar,GPR)作为一种较新的地球物理方法,以其特有优势广泛应用于植物根系的探测.首先介绍了利用探地雷达探测植物根系的基本原理,然后对植物根系的制图、植物根径大小的估算、根系生物量的估算等几个方面的应用进展进行了综述,并从探地雷达系统、根系性质和土壤性质等不同角度探讨了影响探地雷达在植物根系探测中的主要因素,同时指出目前研究中的不足之处,今后的研究工作应侧重于探地雷达探测植物根系的作用机理及提高其在野外真实条件下的探测能力,以期为探地雷达在植物根系探测中应用的深入和推广提供思路.     

石油演化理论与实践（Ⅰ）——石油演化的机理与石油演化的阶段

Mechanism and stagcs are discussed and a schematic diagram suggested for petroleum evolution based on a preliminsry review of the characteristics of some oil and gas bearing areas in China and a comparison of tbe content and nature of paraffins between shallower sediments .(ineluding recent sediments and organisms)and deed rocks (especially source rocks). During the early stage of petroleum evolution, when biochemical agency in shallower sediments plays the dominant role, most of the primary organic material changes into kerogen, with a certain amount of “dry” gas produced. On the other hand, thermal catalytic degradation contributes significantly to the intermediate and late stages of petroleum generation. The main stage of petroleum genesis in source rocks coincides with the late period of early diagenesis, during which the major mcde of occurrence of oilgenerating source matter is kerogen. The major factors controlling petroleum evolution are temperature, time, and the type of mineral catalytic agents and kerogen.The process of petroleum evolution can be divided into the following stages:(1) Oil and gas forming stage: a) Initial methane gas aubstage--the activity of microorganisms was intensive; formation of kerogen and methane took place. b) Low maturity oil substage. This is the main stage of oil generation.Low-matured oil and wet gas generated via the thermal catalytic degradation of kerogen. (2) Oil and gas maturity stage: a) High maturity oil substage. Both the molecular weight of paraffins and the ratio of oil to gas decrease. b) Final methane gas substage. This is the last period of petroleum evolution, with methane and highly matured bitumens as its final products.