盘县砂锅厂金矿大麦地—小尖山矿段褐铁矿化特征及地质意义

盘县砂锅厂金矿大麦地—小尖山矿段产出层位是峨眉山玄武岩组一段下部凝灰岩,为凝灰岩型金矿。在大麦地—小尖山矿段内发育有较多的断裂构造和与黔西南其他金矿区氧化程度相比较为强烈的褐铁矿,褐铁矿多发育在有断裂构造通过地带,充填在节理、裂隙、破碎带中,呈铁壳、脉状、网格状产出。经系统测量统计并做出褐铁矿走向玫瑰花图显示,褐铁矿与断裂构造有着方向上的关系,并且矿段内的矿(化)点与围岩蚀变中的褐铁矿化、硅化关系十分密切。     

西藏拉萨达孜侏罗统叶巴组火山角砾凝灰岩中波痕的发现及意义

文章分析了西藏拉萨达孜侏罗统叶巴组火山角砾凝灰岩的地质背景、波痕及寄主地层特征。结果显示,西藏拉萨达孜叶巴组为一套中酸性火山岩及火山碎屑岩为主的岩石组合,其地球化学特征证实为岛弧环境,其中段火山角砾凝灰岩中发现波痕,波长介于165-235cm,波高约20-30cm,为具宽阔的不对称浪成波痕,其古流向为SSE,形成于滨岸地带。     

三塘湖盆地石炭系埋藏溶蚀型凝灰岩致密油成藏特征

凝灰岩致密油藏作为一种特殊的油藏类型,已受到高度关注,但前人对埋藏成岩阶段形成的凝灰岩致密油藏研究很少。本文通过对三塘湖盆地石炭系哈尔加乌组埋藏溶蚀型凝灰岩致密油成藏条件的研究,明确了成藏主控因素,并建立了成藏模式。研究表明：哈尔加乌组烃源岩有机质丰度较高,有机质类型较好,并处于成熟演化阶段,油源对比表明埋藏溶蚀型凝灰岩油藏中原油来自哈尔加乌组内部烃源岩;埋藏溶蚀型凝灰岩物性较好,溶蚀孔隙为上部烃源岩在演化过程中产生的大量有机酸对储层的溶蚀作用而形成;埋藏溶蚀型凝灰岩油藏的形成主要受哈尔加乌组成熟烃源岩分布、卡拉岗组大套烃源岩下部物性较好的凝灰岩储层及圈闭条件的控制,形成“下部成熟烃源岩供烃、上部有机酸溶蚀形成物性较好凝灰岩储层及有效圈闭存储”多项成藏条件有利配置下的成藏模式。本文研究将对其他地区埋藏溶蚀型凝灰岩油藏的分布与预测提供借鉴。     

云南华丽高速公路隧道大变形处治措施

文笔山隧道在施工中出现大范围的初支结构大变形破坏现象,严重影响工程工期﹒基于工程勘察资料与现场监测数据,结合工程地质和施工条件分析隧道大变形的特征与原因,提出了针对性的大变形处治措施﹒研究表明:对大变形段围岩注浆加固、变形趋稳时重新施做初支结构;对掌子面前方未施工段采取改善超前支护类型、加大预留变形量、增强初支结构强度、加强锁脚连接和强化施工质量等措施﹒后续施工现场情况表明,隧道大变形成功得到控制﹒     

天龙十三

我国是世界上公认的恐龙之乡,其化石分布之厂,属种数量之多,都是独一无二的。但遗憾的是,在所有已被发掘出的恐龙化石中,神态生动、品相完整,且栩栩如生的恐龙群体活埋标本却少而又少。所幸的是,近日笔者在上海一位藏家的手上,见到了一块这种标本。在这块呈椭圆状不足一个平方米的火山凝灰岩上,竟然重重叠叠且又清晰可辨地盘踞着13条鹦鹉嘴龙。     

SHRIMP U-Pb zircon age of tuff at the bottom of the Lower Cambrian Niutitang Formation,Zunyi, South China

A SHRIMP U-Pb zircon geochronology study of the tuff at the bottom of the Lower Cambrian Niutitang Formation at Songlin, Zunyi, South China yielded a mean ^206Pb/^238U age of 518±5 Ma. It is significantly younger than the Re-Os ages of 537--542 Ma for the overlying polymetallic Ni-Mo-PGE-rich layer in the basal Niutitang Formation at Songlin, suggesting that the Re-Os ages might represent that of the original magma chamber for the Ni-Mo-PGE-rich layer rather than the formation age of the strata. The intra-basinal stratigraphic correlation also implies that the absolute age of the Chengjiang biota should be younger than 518±5 Ma. Our new result, together with the SHRIMP U-Pb zircon age for the K-bentonite in the Zhongyicun member of the Zhujiaqing Formation at the Meishucun section, Yunnan Province, provides a temporal constraint for the Lower Cambrian of the Yangtze Platform in South China.     

遵义牛蹄塘组底部凝灰岩锆石SHRIMP U-Pb年龄及其地质意义

制约扬子地台早寒武世地层的精确锆石U-Pb年龄稀少,对最近于遵义松林地区下寒武统牛蹄塘组底部发现的凝灰岩中的锆石斑晶进行SHRIMP U-Pb测年,结果显示凝灰岩的就位年龄为(518±5)Ma(MSWD=0.37),从而提供了扬子地台下寒武统第二个精确锆石U-Pb年龄数据,构建了该区下寒武统以精确锆石U-Pb年龄为基础的时间框架雏形.结合区域地层对比,凝灰岩年龄数据显示澄江生物群及三叶虫首现(FAD)的绝对年龄应该晚于(518±5)Ma.该年龄数据同时表明,遵义松林地区牛蹄塘组底部Ni-Mo-PGE多金属富集层的Re-Os等时线年龄数据(537～542Ma)不代表地层的年龄.     

玻屑凝灰岩合成A型沸石工艺优化研究

以经过预处理的玻屑凝灰岩为原料,采用水热反应晶化合成工艺,并对该工艺进行优化,可合成出质量较好的A型沸石产品.该合成工艺流程为:玻屑凝灰岩(预处理)+氢氧化钠+铝酸钠+水→水热反应→晶化合成→过滤、洗涤→烘干→A型沸石产品.最佳技术参数为:硅铝比为2,钠硅比为1.2,水钠比为45,晶化时间≥6h,晶化温度100℃.该工艺流程简单,技术参数容易控制,原料来源丰富,合成成本低,易于实现工业化生产.图6,表4,参14.     

SHRIMP U-Pb zircon age of tuff from the Kunyang Group in central Yunnan： Evidence for Grenvillian orogeny in South China

Whether or not Grenvillian orogeny occurred in South China still remains highly controversial because high-quality,discriminating data are lacking,and therefore,the key to resolve this matter is to find datable volcanic and/or sedimentary rocks related to Grenvillian orogeny. Such rocks are apparently present in the Fuliangpeng Member from the lower-middle part of Kunyang Group in central Yunnan; here the unit is more than 100 m thick and consists of andesitic ignimbrite,tuffite,terrigeous clastic rocks and carbonates. These volcanic rocks,developed south of the Sibao fold-thrust belts,represent the earliest calc-alkaline volcanic activity in late Precambrian time from central Yunnan and are coeval with both a change in sedimentary facies from detritus to carbonates and the beginning of seismite development elsewhere. Two samples for SHRIMP analysis were collected from this volcanic unit. Sample G3-29-2,from the bottom of Fuliangpeng Member,is an ignimbrite,and about 100 zircon crys-tals recovered from it have euhedral shapes and display relatively simple sector zonation under cathodoluminescent (CL) imaging,suggesting a magmatogenic origin. Twenty-five of the zircons were analyzed and a weighed-mean U-Pb age of 1032±9 Ma was obtained. Sample G3-29-3 from uppermost part of Fuliangpeng Member is a tuffite,and many rounded,evidently detrital zircons were recovered. Nine of these zircons were analyzed,and the oldest single-grain U-Pb zircon age is 1938±26 Ma,im-plying that Paleoproterozoic basement developed in Cathaysia. The dating result,combined with the geotectonic research on the Fuliangpeng Member,leads us to conclude that late Mesoproterozoic orogenic volcanic activity occurred in the western part of South China,and that the related collision of Yangtze and Cathaysian cratons was an integral part of the assembly of Rodinia.