胶东福山北部地区金及多金属成矿系列及找矿方向

胶东福山北部地区位于胶东栖(霞)-蓬(莱)-福(山)成矿带北段。该区粉子山群大面积出露,中生代岩浆活动强烈,褶皱断裂构造发育,形成一完整的热液成矿系统。对区内邢家山(钼钨)、王家庄(铜锌)、杜家崖(金)等典型矿床(式)研究发现,该区金属成矿作用与中生代燕山晚期斑岩体具有密切关系,由高温至低温成矿作用在空间上展布规律明显,共同构成了与中生代燕山晚期中酸性岩浆侵入作用有关的金及多金属成矿系列。从现有研究成果看,中低温热液脉型、斑岩-矽卡岩型以及浅成低温热液型金及多金属矿应作为该区找矿主攻方向。     

南极菲尔德斯半岛潮间带沉积物细菌的多样性及分离菌产酶测定

摘要:南极菲尔德斯半岛具有多种不同特征的生态地理微环境,如长城科考站、企鹅岛、生物湾与黄金湾流域、半岛南部、碧玉滩等。这些区域因水文地质、动植物分布、人类活动程度等不同而具有明显的生态地理差异。本研究从这些微环境海岸潮间带采集了7份代表性沉积物样品,采用16S rRNA基因高通量测序方法,对其细菌类群的多样性以及环境理化因子的影响进行了比较分析;同时采用常规可培养鉴定方法,对样品的分离菌株产酶状况进行了初步测定。结果表明：整体上看,所有样品的细菌类群主要分布在45门、104纲、442属当中,表现出比较高的多样性。其中,优势菌门Proteobacteria主要分布在半岛南部、碧玉滩和生物湾潮间带沉积物物中,优势菌门Bacteroidetes主要分布在企鹅岛两侧和黄金湾潮间带沉积物,长城站潮间带沉积物的优势门为Firmicutes。相似生态微环境的潮间带沉积物具有不同的优势菌门和纲;而不同生态微环境潮间带沉积物却具相同的优势菌门和纲。有机氮（TON）、NH4+-N、NO3--N、PO43--P、NO2--N含量与企鹅岛两侧、生物湾、黄金湾潮间带沉积物的菌群多样性具有相关性,其中TON对生物湾样品的影响最大,而有机碳（TOC）对所有样品的影响较小。分离菌株的产酶实验表明：在企鹅岛、生物湾、黄金湾等动物频繁出没的潮间带样品中,蕴藏着一批产淀粉酶、酪蛋白酶、脂肪酶、七叶苷酶、过氧化氢酶能力较强菌株,这为今后进一步的应用开发提供了宝贵的低温产酶菌株来源。 关键词: 菲尔德斯半岛; 潮间带沉积物; 细菌类群多样性; 产酶菌株     

胶东郭家岭花岗闪长岩U--Pb年代学、地球化学特征及地质意义

郭家岭花岗闪长岩岩石地球化学特征表明其SiO2含量较高,为71.3%~73.28%,K2O=2.14%~4.29%,属于高钾钙碱性--钙碱性I型花岗岩。锆石LA--ICP--MS U--Pb年龄显示郭家岭花岗岩体成岩年龄为127.9±1.3 Ma,属早白垩世。岩石的Rb/Sr和Nb/Ta比值,以及暗色闪长质包体研究表明郭家岭花岗闪长岩为壳幔混合源,岩浆源区为具有幔源特征的新生镁铁质下地壳。结合区域地质分析认为郭家岭花岗闪长岩的形成与太平洋板块俯冲引起的大陆弧伸展作用最密切。     

THE CHARACTERISTIC AND CAUSE OF SEA WATER INTRUSION AND POLLUTION IN SOUTH LIAODONG PENINSULA

Based on various patterns of groundwater and their abundance characters in south Liaodong Peninsula, the distribution, stage, pattern and characters of sea water intrusion in the serious sea water intrusion areas are analysed. The reasons to cause sea water intrusion are uneven precipitation, limited recharge of surface water, artificial overpumping, lithology and geological structure. It can provide scientific basis for reasonable utilization of limited water resource in line with the local conditions.     

渤海湾盆地辽东湾地区古近系地震相研究

对辽东湾地区古近系地层进行了研究,选择了可信度较高的地震反射内部结构和外部形态,辅助地震反射振幅、连续性等参数,对地震相进行了划分命名。在研究区6个地震层序中共识别出平行—亚平行席状地震相、前积地震相、楔状地震相、充填状地震相、透镜状地震相、丘状地震相及乱岗状地震相等多种类型。这些地震相在平面分布上具有差异性,在垂向演化上具有继承性。将地震相转变为沉积相,划分出了湖泊沉积环境的深湖—半深湖、滨浅湖、扇三角洲、近岸水下扇、三角洲、浊积扇等沉积相,预测出了有利沉积相带。     

Genesis of the Maoling gold deposit in the Liaodong Peninsula: Constraints from a combined fluid inclusion,C-H-O-S-Pb-He-Ar isotopic and geochronological studies

The large tonnage Maoling gold deposit (25 t @ 3.2 g/t) is located in the southwest Liaodong Peninsula, North China Craton. The deposit is hosted in the Paleoproterozoic metamorphic rocks. Four stages of mineralization were identified in the deposit: (stage I) quartz-arsenopyrite ± pyrite, (stage II) quartz-gold- arsenopyrite-pyrrhotite, (stage III) quartz-gold- polymetallic sulfide, and (stage IV) quartz-calcite-pyrrhotite. In this paper, we present fluid inclusion, C-H-O-S-Pb-He-Ar isotope data, zircon U-Pb, and gold-bearing sulfide (i.e. arsenopyrite and pyrrhotite) Rb-Sr age of the Maoling gold deposit to constrain its genesis and ore-forming mechanism. Three types of fluid inclusions were distinguished in quartz-bearing veins, including liquid-rich two-phase (WL type), gas-rich two-phase (GL type), and daughter mineral-bearing fluid inclusions (S type). Fluid inclusions data show that the homogenization at temperatures 197 to 372 °C for stage I, 126 to 319 °C for stage II, 119 to 189 °C for stage III, and 115 to 183 °C for stage IV, with corresponding salinities of 3.7 to 22.6 wt.%, 4.7 to 23.2 wt.%, 5.3 to 23.2 wt.%, and 1.7 to 14.9 wt.% NaCl equiv., respectively. Fluid boiling was the critical factor controlling the gold and associated sulfide precipitation at Maoling. Hydrogen and oxygen stable isotopic analyses for quartz yielded δ¹⁸O = ?5.0‰ to 9.8‰ and δ D = ?133.5‰ to ?77.0‰. Carbon stable isotopic analyses for calcite and ankerite yielded δ¹³C = ?2.3‰ to ?1.2‰ and O = 7.9‰ to 14.1‰. The C-H-O isotope data show that the ore-forming fluids were originated from magmatic water with meteoric water input during mineralization. Hydrothermal inclusions in arsenopyrite have ³He/⁴He ratios of 0.002 Ra to 0.054 Ra, and ⁴⁰Ar/³⁶Ar rations of 1225 to 3930, indicating that the ore-forming fluids were dominantly derived from crustal sources almost no mantle input. Sulfur isotopic values of Maoling fine-grained granite range from 6.‰1 to 9.8‰, with a mean of 7.7‰, δ³⁴S values of arsenopyrite from the mineralized phyllite (host rock) range from 8.9‰ to 10.6‰, with a mean of 10.0‰, by contrast, δ³⁴S values of sulfides from ore vary between 4.3‰ and 10.6‰, with a mean of 6.8‰, suggesting that sulfur was mainly originated from both the host rock and magma. Lead radioactive isotopic analyses for sulfides yielded ²⁰⁶Pb/²⁰⁴Pb = 15.830–17.103, ²⁰⁷Pb/²⁰⁴Pb = 13.397–15.548, ²⁰⁸Pb/²⁰⁴Pb = 35.478–36.683, and for Maoling fine-grained granite yielded ²⁰⁶Pb/²⁰⁴Pb = 18.757–19.053, ²⁰⁷Pb/²⁰⁴Pb = 15.596–15.612, and ²⁰⁸Pb/²⁰⁴Pb = 38.184–39.309, also suggesting that the ore-forming materials were mainly originated from the host rocks and magma. Zircon U-Pb dating demonstrates that the Maoling fine-grained granite was emplaced at 192.7 ± 1.8 Ma, and the host rock (mineralized phyllite) was emplaced at some time after 2065.0 ± 27.0 Ma. Arsenopyrite and pyrrhotite give Rb–Sr isochron age of 188.7 ± 4.5 Ma, indicating that both magmatism and mineralization occurred during the Early Jurassic. Geochronological and geochemical data, together with the regional geological history, indicate that Early Jurassic magmatism and mineralization of the Maoling gold deposit occurred during the subducting Paleo-Pacific Plate beneath Eurasia, and the Maoling gold deposit is of the intrusion-related gold deposit type.     

辽东湾红沿河附近海域2017—2018年冬季气温-水温-冰情关系研究

辽东湾是我国冰情最严重海域,每年冬季都会受到海冰的显著影响,冰情预测评估可为辽东湾涉海活动提供防冰抗冰的技术依据。建立气温-水温-冰情的相关性,结合便于获取的现场高精度连续气象数据和高精度冰情预测模型,可实现局地小尺度的冰情快速预测评估。基于2017—2018年冬季辽东湾东岸红沿河附近海域实测气象-水温-冰情同步观测数据,结合辽东湾大尺度整体冰情（浮冰面积）,推演局地气温、水温与不同尺度冰情评价参数（浮冰范围与冰厚）的相关关系,提出基于不同气温区间的气温变化规律的冰底热通量选取方法,进而建立适用于辽东湾的气温-水温-冰情评估方法。相关性分析结果显示：观测点气温与水温存在明显相关性;浮冰范围与气象数据存在明显相关性,临界温度为 -5 ℃的累计负气温能很好拟合本年度盛冰期浮冰范围。基于HIGHTSI进行数值模拟后发现：水温与块体积法计算冰底热通量时,冰水间的热传递系数取2.2×10^-5是可行的;水温对冰情的影响表现在海冰冰厚最大值与冰期长短。为弥补辽东湾其他海域因缺少实测海水温度观测数据欠缺、冰底热通量选取不准选取导致的冰情模拟预测评估困难的问题,本文依据水温与气温的相关性,将水温随气温变化划分为结冰区（气温小于-10 ℃时水温维持冰点附近）、过渡区（气温为-10~-5 ℃时水温处于-1.4~-0.4 ℃）、融冰区（气温高于-5 ℃时水温随气温的增大逐渐增大）,进而提出适用于辽东湾所有海域的冰底热通量计算方法和冰情评估方法。     

辽南上达子堡金矿化区黄铁矿标型特征及意义

上达子堡金矿化区主要出露古元古界辽河群盖县岩组二岩段,是金成矿物质的矿源层。黄铁矿标型特征指示目前区内的剥蚀水平相当于中上部,按黄铁矿垂直分带规律,{210}+{100}、{210}习性晶体向深部有可能逐渐增加,因此,本金矿化区深部含金量可能高于浅部。     

华北克拉通辽东半岛新元古代早期基性岩浆活动:辉绿岩墙年代学和岩石地球化学证据

华北克拉通辽东半岛地区广泛发育侵位于青白口系不同层位中的辉绿岩(脉)岩墙,对其锆石CL图像、U--Pb定年和岩石地球化学特征研究得出以下结论。锆石类型有三组:前两组锆石具有早期岩浆作用的锆石属性或结晶基底的变质锆石属性,反映该区辉绿岩岩浆上升过程受到了陆壳的混染;第三组锆石多呈自形--半自形短柱状,发育岩浆振荡生长环带结构或条带结构,具原生岩浆成因锆石属性,锆石SHRIMP U--Pb定年显示其加权平均年龄为832.3±8.1 Ma(n=14,MSWD=1.3),可以代表辉绿岩的结晶年龄。岩石地球化学组成,其具有低Si O_2、Al_2O_3,高TFe_2O_3、MgO、Ti O_2的特征,这与拉斑玄武岩特征相似;其稀土元素总量相对较低(ΣREE=71.88×10~-6~129.64×10~-6),且具弱的正Eu异常和铌亏损;略富集轻稀土元素(LREE)、富集大离子亲石元素(LILE:Rb、Pb、Ba)和高场强元素(HFSE:Th、U、Zr、Ti、Hf),而亏损高场强元素(HFSE:Nb、Sm、Gd、P)等;以上特征指示岩浆源区为富集型地幔,且上侵位就位过程中受陆壳不同程度的同化混染。本文对辉绿岩的研究显示华北克拉通辽东半岛地区在新元古代早期存在基性岩浆活动,结合前人对华北克拉通中元古代晚期—新元古代早期构造--岩浆事件的研究成果,进一步证明了华北克拉通东北部在新元古代早期经历了挤压汇聚后的伸展裂解演化过程,这与Rodinia超大陆聚合和裂解事件一致。     

王冠头虫的卷曲

笔者(1987,1988)在辽东半岛南部复州湾晚寒武世崮山组中发现卷曲的王冠头虫。卷曲的王冠头虫的卷曲器官为胸节和尾节,其中最重要的是胸节和尾节中轴的半环。三叶虫的卷曲显示了生物力学的作用,卷曲是生物与环境相适应的表现,由环节动物的侧曲到节肢动物三叶虫的卷曲是生物演化的规律。