Geochemical and Petrological Studies on the Early Carboniferous Sidingheishan Mafic–Ultramafic Iintrusion in the Southern Margin of the Central Asian Orogenic Belt, NW China

The Sidingheishan mafic-ultramafic intrusion is located in the eastern part of the Northern Tianshan Mountain, along the southern margin of the Central Asian Orogenic Belt in northern Xinjiang autonomous region of China. The Sidingheishan intrusion is mainly composed of wehrlite, olivine websterite, olivine gabbro, gabbro and hornblende gabbro. At least two pulses of magma were involved in the formation of the intrusion. The first pulse of magma produced an olivine-free unit and the second pulse produced an olivine-bearing unit. The magmas intruded the Devonian granites and granodiorites.An age of 351.4±5.8 Ma(Early Carboniferous) for the Sidingheishan intrusion has been determined by U-Pb SHRIMP analysis of zircon grains separated from the olivine gabbro unit. A U-Pb age of 359.2±6.4 Ma from the gabbro unit has been obtained by LA-ICP-MS. Olivine of the Sidingheishan intrusion reaches 82.52 mole% Fo and 1414 ppm Ni. On the basis of olivine-liquid equilibria, it has been calculated that the MgO and FeO included in the parental magma of a wehrlite sample were approximately10.43 wt% and 13.14 wt%, respectively. The Sidingheishan intrusive rocks are characterized by moderate enrichments in Th and Sm, slight enrichments in light REE, and depletions in Nb, Ta, Zr and Hf. The ε_(Nd)(t) values in the rock units vary from +6.70 to +9.64, and initial ~(87)Sr/~(86)Sr ratios range between 0.7035 and0.7042. Initial ~(206)Pb/~(204)Pb, ~(207)Pb/~(204)Pb and ~(208)Pb/~(204)Pb values fall in the ranges of 17.23-17.91,15.45-15.54 and 37.54-38.09 respectively. These characteristics are collectively similar to the Heishan intrusion and the Early Carboniferous subduction related volcanic rocks in the Santanghu Basin, North Tianshan and Beishan area. The low(La/Gd)_(PM) values between 0.26 and 1.77 indicate that the magma of the Sidingheishan intrusion was most likely derived from a depleted spinel-peridotite mantle.(Th/Nb)_(PM)ratios from 0.59 to 20.25 indicate contamination of the parental magma in the upper crust.Crystallization modeling methods suggest that the parental magma of the Sidingheishan intrusion was generated by flush melting of the asthenosphere and subsequently there was about 10 vol%contamination from a granitic melt. This was followed by about 5 vol% assimilation of upper crustal rocks. Thus, the high-Mg basaltic parental magma of Sidingheishan intrusion is interpreted to have formed from partial melting of the asthenosphere during the break-off of a subducted slab.     

豫西崤山东部中河岩体锆石U-Pb年龄、地球化学和Lu-Hf同位素特征

中河花岗斑岩体位于河南省崤山东部,该岩体是最近发现的中河大型银铅锌矿床的成矿母岩。选取2件花岗斑岩样品进行LA-ICP-MS锆石U-Pb定年,获得2件样品的~(206)Pb/~(238)U年龄加权平均值分别为(129±0.7)Ma(MSWD=0.78)和(131±1.5)Ma(MSWD=1.70),表明中河岩体形成于早白垩世。岩石地球化学特征显示,中河岩体具有高的w(SiO_2)和w(K_2O)、低的w(Na_2O),其A/CNK比值为1.03~1.63,Mg#值介于25~50,总体上属于过铝质-强过铝质的高钾钙碱性系列。岩石具有低的w(Yb),中等-弱的铕负异常,稀土元素配分曲线为轻稀土元素富集型,轻稀土元素分馏相对强烈,但重稀土元素分馏不明显。中河岩体有相对低的w(Sr)和w(Y),且富集大离子亲石元素Rb、Ba、U、K和轻稀土元素,亏损高场强元素Nb、Ta、P、Zr、Hf、Ti和重稀土元素。中河岩体锆石εHf(t)值为-34.4~-23.2,平均为-26.9,Hf同位素二阶段模式年龄介于2485~3182 Ma,平均为2714 Ma。岩石地球化学特征及Hf同位素组成表明中河岩体的岩浆源区主要为新太古代地壳物质,并有少量的中太古代地壳物质,中-新太古代增生的具有弧岩浆特征的地壳物质部分熔融形成了早白垩世的中河岩体。     

西秦岭中—晚三叠世构造属性:来自将其那梁侵入杂岩体的年代学及地球化学证据

西秦岭造山带印支早期的构造环境仍存在较多争论,选择西秦岭将其那梁杂岩体进行详细的年代学、岩石学及地球化学分析,以期对该科学问题进行深入探讨。将其那梁杂岩体由石英闪长岩和花岗斑岩组成,石英闪长岩LA-ICP-MS锆石U-Pb年龄为(240.0±1.5) Ma,形成时代为中三叠世,属于早印支期。将其那梁杂岩体具有富钾(K₂O=3.09%~3.54%)、富碱(K₂O+Na₂O=6.44%~7.20%)和过铝质(A/CNK=1.05~1.56)特征,Mg^#值(54~67)较高,属于过铝质高钾钙碱性岩类。将其那梁杂岩体石英闪长岩和花岗斑岩具有相似的微量元素及稀土元素组成,轻重稀土元素分馏明显(LREE/HREE=8.19~14.63),呈右倾特征,显示无或弱负Eu异常(δEu=0.87~1.03),具有亏损Nb、Ta、Zr等高场强元素和富集Ba、Rb、Sr等大离子亲石元素的地球化学特征。岩石地球化学特征指示,将其那梁杂岩体主要源于下地壳高钾变基性岩的部分熔融,且有幔源物质参与其中。结合区域地质背景,认为将其那梁杂岩体形成于火山弧构造环境,可能与中—晚三叠世阿尼玛卿—勉略洋向北俯冲有关,反映了中—晚三叠世西秦岭地区具有活动大陆边缘的属性。     

晚中生代沂沭断裂带左旋韧性剪切与岩浆迁移规律

沂沭断裂带内部的岩浆侵入与断裂活动关系密切,开展沂沭断裂带内部岩浆年代学研究,对于沂沭断裂带构造背景研究具有积极的参考意义。选取沂沭断裂带内部的莒县浮来山正长岩体、边部的莒南官坊石英正长岩体及侵入该岩体的闪长玢岩脉,开展岩石学及年代学研究。首次发现晚中生代沂沭断裂带左旋韧性剪切,获得浮来山岩体的LA-ICP-MS锆石U-Pb年龄为(125.1±1.7) Ma,官坊岩体年龄为(125.6±2.0) Ma, 发生韧性变形的闪长玢岩脉年龄为(122.8±2.1) Ma。获得的125 Ma岩浆活动年龄与沂沭断裂带东侧的五莲变质核杂岩快速剥露(122~128 Ma)、诸城断陷盆地快速沉降的时间相吻合,该时期沂沭断裂带处于岩石圈减薄与破坏强烈的时期;闪长玢岩脉的122.8 Ma结晶年龄,与五莲变质核杂岩后构造岩体(石场、坊子岩体等)结晶年龄一致,该时期沂沭断裂带处于弱伸展状态,同时也说明胶东半岛岩石圈减薄具有时间上的一致性。晚中生代时期,沂沭断裂带两侧岩浆活动具有逆时针迁移的规律,这一规律可能与伊佐奈岐板块向欧亚板块俯冲的方向、角度、速度的变换有关。     

Southwestward intrusion of korea strait bottom cold water observed in 2003 and 2004

Hydrographic surveys were carried out four times in the western channel of the Korea Strait in March and August 2003 and in June and November 2004. The bottom cold water, which was lower than 10°C, appeared in the channel trough except in March 2003. It flowed southwestward along the shelf of Korean coasts in August 2003 and in November 2004. The width and the maximum speed of the intrusion current were about 20 km and approximately 25 cm s^-1, respectively, off Ulsan, Korea. The volume transport of the bottom cold water was estimated 0.019 Sv (Sv≡10⁶ m³ s^-1) in August 2003 and 0.026 Sv in November 2004.     

伽师强震群的深部动力学条件

根据天山造山带及其两侧的塔里木盆地和准噶尔盆地的岩石圈二维速度结构、二维密度结构、二维电性结构、壳幔过渡带的详细结构以及大地热流和震源深度的分布,再结合对新疆西北部的蛇绿岩带、高压变质带和岩浆岩分布的综合分析,建立了天山造山带的地球动力学“层间插入消减”模型。该模型认为,塔里木板块的中上地壳在库尔勒断裂附近向天山造山带的中下地壳层间插入;而下地壳连同岩石圈地幔向天山造山带的上地幔俯冲消减。在天山的西段（哈萨克斯坦境内）,费尔干纳地块由北向南插入到南天山之下约180km的深处,在其东段（中国境内）,塔里木盆地由南向北插入南天山之下。这两个具有不同方向的下降板片的接触部位为费尔干纳走滑断裂。我国的伽师、喀什、乌恰地震区均落在这两个具有不同俯冲方向板块的结合部位附近,有着特殊的深部构造背景。南、北两大板块的双向挤压必定产生强大的应力,在地震区附近,这种应力的积累与释放具有4个显著的特点：（1）板片的俯冲消减速度约高达每年22mm左右;（2）应力的积累与释放速率加快;（3）应力释放较容易;（4）应力释放较为集中。这4个特点可能是伽师地区在较短的时间内连续发生数次强震的构造因素。     

龙首山几个镁铁-超镁铁质岩体比较

文章选择龙首山隆起区金川、塔马子沟、毛草泉、小口子、藏布台几个镁铁-超镁铁质岩体进行地质、地球化学比较研究,发现岩体普遍具有橄榄石堆晶特征,中段金川岩体以二辉橄榄岩为主要特征,外围岩体以单辉橄榄岩为特征.地球化学数据显示,这些镁铁-超镁铁质岩体处于相同的岩石系列,源区具有相似性,岩体含矿差异主要源自岩浆演化.结合地质综合场模型,提出金川外围岩体在龙首山隆起区,沿构造带东西长约80～100km范围存在金川深部岩浆房响应的产物.     

1617号鲇鱼台风登陆后引发不同性质暴雨的成因对比分析

2016年9月28日1617号台风"鲇鱼"登陆后由台风本体环流和外围环流引发了不同性质的暴雨,这是本次秋季登陆台风暴雨预报的难点。利用常规气象观测资料以及NCEP的1°×1°再分析资料等,对不同性质暴雨的成因进行了诊断对比分析。结果表明:浙江东南部对流性降水和江西南部稳定性降水的大气层结结构具有明显的差异。中高纬度低槽距离台风较远,冷空气主要从低层入侵台风西北侧,破坏台风低层的暖心结构。台风外围中层干冷空气随东南风向浙江东南部输送,并叠加在低层暖湿气流之上,形成上冷下暖的不稳定层结,同时在对流层上层有干冷空气下沉至台风环流中下层(干侵入),导致浙江文成附近出现了局地特大暴雨。江西南部由于低层被湿冷空气占据,层结较为稳定,降水发展平缓。低空东南急流为台风外围环流暴雨提供了充足的水汽,浙江东南部地形对降水起到了增幅作用。不稳定层结及中层冷空气的输送对对流性暴雨的激发作用可以为登陆台风降水性质和强度预报提供参考依据。     

Zoning and layering in diorites of the scottish caledonian appinite suite

Dioritic plugs (< 1 km across) are common associates of the late Caledonian, post-tectonic granites of the Scottish Highlands. These contain a very wide range of rock types from ultramafic through mesocratic diorites to anorthositic and granitic. These rocks form steeply dipping, wall-parallel layers and zones within the plugs. Outer layers are shown to form first, inner layers later. Mafic zones are composed of the minerals seen as phenocrysts in chilled margins and have the chemical characteristics of cumulates. The inner margins of the mafic zones reflect the onset of plagioclase crystallization. Core zones also show inward variations in mineralogy and texture which define vertical, wall-parallel cylinders. These variations are ascribed to fractional crystallization accompanying accretion of rock onto the pipe walls. Cores in different intrusions may be mafic, mesocratic, or leucocratic, which indicates vertical zonation in the bodies. The mafic cores additionally show that recharge with less evolved magma occurred in some cases. The few larger (> 1 km diameter) intrusions show examples of layering and lamination dipping at low to moderate angles. These indicate the beginning of a change from wall-dominated to floor-dominated crystallization as intrusion diameter increases. A comparison is made with the nature and origin of layering in other intrusions.     

海口湾的溶解氧及海水水质指标限制值问题

海水溶解氧对海洋生物的生存、生长和发育相当重要,与生物活动有着密切的联系,它的含量变化是反映生物生长状况的一个重要标志,同时也是污染监测的重要指标.海口湾是海南省的重点海域,1989年以来,陈春华等对海口湾的环境问题进行了大量的研究[1~6],本论文就海口湾的溶解氧监测结果进行分析,并发现了溶解氧水质标准限制值存在的问题.每年在该湾布设10余个站点进行污染监测,有必要对海口湾近7年监测结果进行综合分析.