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911.
912.
鸡南铁矿床位于吉林省和龙地区,地处华北克拉通北缘与兴蒙造山带接壤的龙岗地块北部,是东北地区发现较早的BIF型铁矿床之一。该矿床铁矿体主要呈层状、似层状、扁豆状赋存于鞍山群鸡南组上段中部层位,含矿岩石以黑云斜长片麻岩、角闪黑云斜长片麻岩、黑云角闪斜长片麻岩及斜长角闪岩为主,为角闪岩相的中低级区域变质岩系;主要矿石类型为条带状磁铁石英岩型和块状磁铁角闪岩型。为确定该矿床含矿建造的原岩、变质时代及构造背景,重点对含矿岩系中的斜长角闪岩进行了岩石地球化学和锆石U-Pb年代学研究。结果表明：斜长角闪岩的地球化学特征表现为富集大离子亲石元素、轻微富集重稀土元素;主量元素质量分数与中性-基性岩类基本相似,结合原岩恢复图解,判断其原岩类型为亚碱性玄武岩（拉斑玄武岩）,形成于弧后盆地背景;LA-ICP-MS锆石U-Pb年代学研究中,2个较老的锆石测点年龄分别为（2 468±15）和（2 469±9）Ma,代表区内峰期变质年龄（约2 460 Ma）,26个锆石测点的测年数据较为集中,加权平均年龄为（2 275±25）Ma,代表区内退变质年龄。通过与国内外典型BIF型铁矿床的对比研究认为,区内的鸡南铁矿与官地铁矿同属Algoma型铁矿床。 相似文献
913.
白钨矿是各类矿床中较为常见的副矿物,通过分析白钨矿的稀土元素质量分数及其标准化配分模式图,可为矿床成矿流体特征及演化提供重要的判别依据。本文对东北地区羊鼻山矽卡岩型矿床和杨金沟热液脉型矿床两个典型钨矿床的白钨矿样品中的稀土元素进行了激光剥蚀-电感耦合等离子体质谱（LA-ICP-MS）原位分析。其中：羊鼻山矽卡岩型矿床白钨矿LA-ICP-MS分析方法所获得的稀土元素配分曲线模式与前人用传统的溶液-ICP-MS分析方法所获得的结果完全吻合,表明采用剥蚀束斑44 μm和剥蚀频率7 Hz的193 nm ArF激光器,NIST 610作外部标样,Ca作内标元素,对基体效应影响最小,所获数据可靠,方法可行;而杨金沟热液脉型矿床白钨矿溶液-ICP-MS分析方法与LA-ICP-MS分析法所获得结果既具有相似性又具有差异性。原因在于羊鼻山白钨矿的成因类型为矽卡岩型、粒度较小且形成时间短,因此不同矿物颗粒间、同一矿物不同部位间稀土元素的配分模式一致;而杨金沟白钨矿的成因类型属于热液脉型、粒度较大、沉淀结晶时间长,因此同一矿物不同部位的稀土元素的配分模式因成矿流体早晚阶段不同而不同。基于以上对比研究发现,无论是在取样和测试过程方面,还是数据准确度方面,相比传统溶液-ICP-MS分析法,LA-ICP-MS原位分析法均具有明显的优势,主要表现在样品形式简单、粒度和质量分数要求低、测试周期短、费用低且结果精确度高;同时其可对不同成矿阶段或白钨矿不同部位成分进行精细测定,从而得出不同成矿阶段或白钨矿不同部位的稀土元素质量分数,以及在更高的空间分辨率下获得更详细准确的数据信息。此外,对白钨矿（尤其是无明显环带者）进行LA-ICP-MS原位分析时,既可采用电子探针微量分析（EPMA）准确测定Ca的质量分数,也可直接采用标准化学式计算Ca的质量分数,分析所得数据同样可以获得合理的地质解释。 相似文献
914.
Guang-ming Li Kelly Heilbronn Li Zhang Ming-hua Ren Wei Liang Yi-yun Wang Yong Huang Zuo-wen Dai 《China Geology》2020,3(3):369-384
Although some porphyry-skarn deposits occur in post-collisional extensional settings, the post-collisional deposits remain poorly understood. Here the authors describe the igneous geology, and mineralization history of Tuolangla, a newly-discovered porphyry-skarn Cu-W-Mo deposit in southern Tibet that belongs to the post-collisional class. The deposit is associated with Lower Cretaceous Bima Formation. It was intruded by granodiorite porphyry intrusions at about 23.1 Ma. Field investigation indicated that mineralization is spatially and temporally associated with granodiorite porphyry. Molybdenite yielded a Re-Os weighted mean age of 23.5 ± 0.3 Ma and is considered to represent the age of skarn mineralization at the deposit. The δ34S values of sulfides, concentrated in a range between 0.6‰ to 3.4‰, show that the sulfur has a homogeneous source with characteristics of magmatic sulfur. The Pb isotopic compositions of sulfides indicate that ore-forming metal materials were derived from the mantle and ancient crust. The granodiorite porphyry displays high SiO2 (68.78%–69.75%) and K2O (3.40%–3.56%) contents, and relatively lower Cr (2.4×10-6–4.09×10-6), Ni (2.79×10-6–3.58×10-6) contents, and positive εHf(t) values (7.7–12.9) indicating that the mineralization porphyry was derived from the partial melting of juvenile lower crust. The Tuolangla deposit is located in the central part of Zedang terrane. This terrane was once considered an ancient terrane. This terrane is in tectonic contact with Cretaceous ophiolitic rocks to its south and Mesozoic continental margin arc volcanics and intrusions of the Gangdese batholith of the Lhasa terrane to its north. Thus, the authors proposed that the Oligocene porphyry skarn Cu-W-Mo mineralization is probably associated with the Zedang terrane. This finding may clarify why the Oligocene (about 23 Ma) deposits are found only in the Zedang area and why mineralization types of the Oligocene mineralization are considerably different from those of the Miocene (17–14 Ma) mineralization. 相似文献
915.
North Carnarvon Basin is a gas province with minor oily sweet spots in deepwater area with water depth more than 500 m, which is one of the hot spots of global petroleum exploration for its series of giant hydrocarbon discoveries in recent years. However, the degree of oil and gas exploration in deepwater area is still low, and the conditions for oil and gas accumulation are not clear. Based on the current exploration situation and latest database of fields, applying multidisciplinary analysis of hydrocarbon geology, hydrocarbon accumulation elements and its exploration direction of North Carnarvon Basin in deepwater area are analyzed. The results show that there are three sets of main source rocks in deepwater area of North Carnarvon Basin, which are Triassic marine shale in Locker Formation and delta coal-bearing mudstone with thin carbonaceous mudstone in Mungaroo Formation, Lower –Middle Jurassic paralic carbargilite and coal measure strata in Athol Formation and Murat Formation, Cretaceous delta mudstone in Barrow Group and marine shale in Muderong Formation. Most source rock samples show gas-prone capability. The coarse sandstone of delta facies in Middle–Upper Triassic Mungaroo Formation is the most important reservoir in deepwater area, Lower Cretaceous Barrow Group deep-water gravity flow or underwater fan turbidite sandstone is the secondly main reservoir. Lower Cretaceous marine shale in Muderong Formation is most important regional caprock. Triassic mudstone in Mungaroo Formation is an important interlayer caprock in deepwater area. There are two main reservoir accumulation assemblages in deepwater area, one is Triassic structural-unconformity plane reservoir accumulation assemblage of Locker Formation to Mungaroo Formation, and the other is Lower–Middle Jurassic Athol Formation and Murat Formation–Lower Cretaceous stratigraphic lithology-structural reservoir accumulation assemblage of Barrow Group to Muderong Formation. There are three main control factors of hydrocarbon Accumulation: One is coupling of source and seal control hydrocarbon distribution area, the second is multi-stage large wave dominated deltas dominate accumulation zone, the third is direction of hydrocarbon migration and accumulation in hydrocarbon-rich generation depression was controlled by overpressure. The south of Exmouth platform in deepwater area is adjacent to hydrocarbon rich depression zone, reservoir assemblage is characterized by “near source rocks, excellent reservoir facies, high position and excellent caprocks ”, which is the main battlefield of deepwater oil and gas exploration in North Carnarvon Basin at present. There are a lot of fault block traps in the northern structural belt of Exmouth platform, and the favorable sedimentary facies belt at the far end of delta plain in Mungaroo Formation is widely distributed, which is the next favorable exploration zone. The Lower Cretaceous, which is located at the concave edge uplift adjacent to the investigator depression and the Exmouth platform, also has a certain exploration prospect in northwest of deepwater area. 相似文献
916.
As in-situ observations are sparse,targeted observations of a specific mesoscale eddy are rare.Therefore,it is difficult to study the three-dimensional structur... 相似文献
917.
论文采用“概率—损失”二维风险模型解构陕西省区域生态风险,基于地貌分区视角识别多源风险类型的同时以景观格局与生态系统服务价值为关联要素合成潜在生态损失,在此基础上分析了陕西省2000—2015年单一风险要素及区域生态风险的时空分异,并基于地貌分区视角结合重心模型探讨了生态风险的时空迁移。结果如下：① 2000、2015年陕西省多源危险度分别为0.3837、0.4558,上升18.79%,大致呈现南北高、中间低的空间格局,沿南北轴线呈现“W型”展布;潜在生态损失分别为0.5537、0.6270,上升13.24%,除高原南部与秦岭东部山区外,生态损失均呈现高值;区域生态风险分别为0.2429、0.2865,上升17.95%,空间上呈现“三高夹两低”的分布格局。② 从时序变化来看,秦巴山地保持较低风险且风险变化率较小;黄土高原与风沙过渡区变化率处于中等,后者面临较高风险;汉江盆地风险最高,该区域与关中平原分别为风险变化率的首位与次位。从生态风险重心变化趋势看,黄土高原与风沙过渡区重心均向西南移动,关中平原与秦岭山地重心东移趋势明显,汉江盆地与大巴山地重心跃向东南。 相似文献
918.
919.
大型海藻龙须菜(Gracilaria lemaneiformis)规模栽培具有重要的经济和环境效益, 但藻体的凋落分解会对栽培区和邻近海域水环境造成一定影响。为探讨龙须菜凋落对水环境的影响, 本文通过45d的室内受控实验, 评估了龙须菜凋落分解过程中水体溶解氧和氮、磷的含量变化。结果发现, 干龙须菜实验组在实验期内水体溶解氧浓度显著降低(较对照组降低了82.81%); 水体氮、磷浓度显著提高, 总氮、总磷浓度较对照组分别上升了161.78%和759.93%。鲜龙须菜+海水+沉积物组在实验前中期(第0~21天)水体溶解氧浓度持续降低(较对照组降低了53.92%), 但在21d后又逐渐恢复至对照组水平; 其水体氮、磷浓度在实验中末期亦显著提高, 分解过程总氮、总磷浓度分别较对照组上升了36.65%和177.80%, 水体氮、磷变化曲线较干龙须菜组平缓且迟滞。鲜龙须菜凋落分解过程中的营养盐释放率低于干龙须菜, 沉积物对鲜龙须菜的分解及氮、磷和碳释放有促进作用, 但对干龙须菜的分解及氮、磷和碳释放有一定程度的减缓作用。龙须菜失重率、分解速率及营养盐释放率均呈现如下规律: 干龙须菜+海水组>干龙须菜+海水+沉积物组>鲜龙须菜+海水+沉积物组>鲜龙须菜+海水组。依据上述结果, 建议在龙须菜规模栽培和收获过程中应及时打捞脱落或衰老藻体, 尤其对已收获的大型海藻应妥善处理, 避免大型海藻腐烂而导致水体污染。 相似文献
920.
甘肃黑方台黄土经历长期的灌溉入渗破坏了其原生结构,改变了不同深度黄土的颗粒级配,影响了土体的力学性质。为研究反复灌溉入渗对坡体的影响,通过室内土柱渗透试验研究了反复入渗对甘肃黑方台黄土渗透特性的影响,并研究了渗透作用下黄土中细颗粒运移的规律与模式。研究表明:①水力梯度对渗透速率影响较小而干密度对渗透速率影响较大;随着入渗次数的增加,重塑黄土的渗透性能变弱;②黄土在渗流力的作用下,存在细颗粒沿渗流方向运移的现象,且细颗粒在土柱中上部聚集最多;③影响细颗粒运移的因素有:水力梯度、干密度和渗透次数;其中细颗粒的运移量与水力梯度、渗透次数呈正相关,与干密度呈负相关,且水力梯度是影响细颗粒运移的主要因素;④在渗透过程中,细颗粒运移堆积,最终填充土体内孔隙,导致黄土的渗透性下降。 相似文献