碳酸盐岩储层的构造控制热液蚀变

本期（2006年11期）《AAPG Bulletin》专辑的内容是碳酸盐岩及其储层的构造控制热液蚀变。这种蚀变涉及碳酸盐主岩的一系列岩相变化，包括硫化物矿床、热液白云岩和淋溶石灰岩，它在很多情况下都会对储层的类型、几何形态、性能和分布产生重大影响。在北美地区，热液白云岩（HTD）储层的勘探和开发已有很长历史，其最早的油气发现是在美国东北部的奥陶系莱马-印第安纳（Lima-Indiana）和其它构造带（Hurley和Budros，1990；Wickstrom等，1992），而目前在美国东北部和加拿大东部的密歇根盆地和阿巴拉契亚盆地北部的特伦顿-布莱克里弗（Trenton-BlackRiver）成藏层带及其他层位，仍继续有油气发现。     

山西塔儿山地区金成矿的构造控制因素

本文通过分析晋南塔儿山地区的构造特征，探讨了该区金成矿作用的构造控制因素。     

川西北三叠系地层中金矿床的矿石建造特征及其成因

川西北三叠系地层中金矿床的矿石建造特征及其成因周渝峰，郑明华，刘建明（成都理工学院）川西北地区自２０世纪８０年代初以来，在三叠系地层中相继发现了东北寨、桥桥上、哲波山、团结和马脑壳等一批微细浸染型金矿床，成为我国此类金矿重要富集区之一。一、地质简况本...     

煤层气地质演化历史数值模拟方法研究

根据前人成果，建立了煤层气地质演化史模型并以此为基础研制了计算机模拟系统。通过对具体地区的实际模拟，总结出了煤层气地质演化史数值模拟研究的方法。整个模拟研究过程包括4个步骤：基础数据提取、计算机模拟研究、模拟结果数据处理和分析、煤层气地质演化史恢复。     

南桐矿区龙潭煤系热演化及煤变质研究

川东地区二叠系龙潭煤系煤变质分带与褶皱关系密切，背斜部位变质浅，向斜部位变质深，且变化急剧．在对南桐矿区重点研究的基础上，用沉积速率比值法和沉积趋势法恢复了川东地区各时期的沉积厚度以及褶皱运动前后龙潭煤系的热演化史，并用Ｈｏｏｄ法确定了煤变质阶段，对川东的煤变质规律作出了合理的解释。     

Preparation and electrochemical performance of nanosized Co3O4 via hydrothermal method

The hydrotalcite-type cobalt compounds were prepared through oxidation of Co（OH）2 gel using NH4OH as precipitating agent and H2O2 as oxidant. These hydrotalcite-type cobalt compounds were transformed into Co3O4 through hydrothermal decomposition with nanostructural deformation. The precursor and product were characterized by Fourier-transform infrared（FT-IR） spectrum, X-ray diffractometry（XRD） and transmission electron microscopy（TEM）. The electrochemical performances of as-prepared nanosized Co3O4 as anode materials in lithium-ion batteries were tested by charge-discharge test in the voltage range of 0-3.0 V. The influence of morphology of Co3O4 particle on the capacity and cycling performance was studied. The results show that the shape and size of the final product can be controlled by altering cobalt sources. The irregular cubic Co3O4 with the average particle size of about 10 nm shows the best electrochemical performance. After 10 charge-discharge cycles, the specific charge capacity retains 555 mA.h/g.     

南水北调邢石段弧形闸门埋件融冰设计

针对南水北调总干渠四季输水的要求和弧门冬季运行的设计工况,采用了以超导液为传热介质、以电加热管和电加热器为加热源的新型电加热融冰装置。从融冰设备的工作原理、融冰设备的结构与布置、组装与试验及融冰设备的保温等方面分别进行了阐述,为有冬季运行需要融冰的工程提供了设计实例。     

鄂西-湘西北地区铅锌矿矿源层对铅锌矿床产出定位的制约

自鄂西至湘西北一线,自北至南铅锌矿的产出层位逐渐抬高。通过对该区矿源层的分析研究发现,矿源层层位控制了铅锌矿的产出层位,北部鄂西地区矿源层为震旦系下统陡山沱组含泥碳质碎屑岩,南部湘西地区矿源层为寒武系下统牛蹄塘组含泥碳质碎屑岩。以地层不整合界面和盆地演化的充填系列为成矿单元,下部碎屑岩地层中的铅锌矿源层制约了上部碳酸岩地层中的铅锌矿的产出定位,矿床就位是热液、矿源层、导矿构造、储矿空间、屏蔽层等多因藕合、临界转换的结果,其成因为盆源热液矿床。     

Hydrothermal preparation and crystal habit of X-zeolite powder

The preparation of X-zeolite powder was investigatedin hydrothermal system, the crystal growth process of X-zeolite in hydrothermal condition was characterized by means of X-ray diffraction, scanning electron microscope and infrared ray. The results show that X-zeolite powder with uniform granularity and intact crystal shape can be obtained in hydrothermal system of acid-treated stellerite-NaOH-NaAl(OH)4-H2O; the crystallite size is in the range of 2 - 3μm. The best reaction time of hydrothermal preparation is 6 h. The formation phases of X-zeolite crystal are as follows: dissolution of feedstocks → formation of [SiO4]4- and [AlO4]5- tetrahedron, many-membered ring,β cage → formation of crystal nucleus and nano-particle → aggregation growth of nano-particle → coalescence growth of crystallite. The crystal habits of X-zeolite are intimately related with crystallization orientation ofβ cage in crystal and with its coupling stability on every crystal face family.