浙江原发性产业集群的形成机制与持续发展

原发性产业集群是浙江省产业发展的主要模式，是在开放的环境中自发形成的。独特的区域“文化基因”，产业特定性知识，产业氛围与地方政府的促进作用是原发性产业集群形成的主要因素；小企业大群落，区内企业的分工协作与竞争，产品的多样化与差别化及集体学习是其主要特点；生产要素的培育和创造，区域品牌树立，学习型企业群落创建及特色制造业基地的培育是产业集群区持续发展的主要措施。     

Infiltration on mountain slopes: a comparison of three environments

Water is well established as a major driver of the geomorphic change that eventually reduces mountains to lower relief landscapes. Nonetheless, within the altitudinal limits of continuous vegetation in humid climates, water is also an essential factor in slope stability. In this paper, we present results from field experiments to determine infiltration rates at forested sites in the Andes Mountains (Ecuador), the southern Appalachian Mountains (USA), and the Luquillo Mountains (Puerto Rico). Using a portable rainfall simulator–infiltrometer (all three areas), and a single ring infiltrometer (Andes), we determined infiltration rates, even on steep slopes. Based on these results, we examine the spatial variability of infiltration, the relationship of rainfall runoff and infiltration to landscape position, the influence of vegetation on infiltration rates on slopes, and the implications of this research for better understanding erosional processes and landscape change.Infiltration rates ranged from 6 to 206 mm/h on lower slopes of the Andes, 16 to 117 mm/h in the southern Appalachians, and 0 to 106 mm/h in the Luquillo Mountains. These rates exceed those of most natural rain events, confirming that surface runoff is rare in montane forests with deep soil/regolith mantles. On well-drained forested slopes and ridges, apparent steady-state infiltration may be controlled by the near-surface downslope movement of infiltrated water rather than by characteristics of the full vertical soil profile. With only two exceptions, the local variability of infiltration rates at the scale of 10° m overpowered other expected spatial relationships between infiltration, vegetation type, slope position, and soil factors. One exception was the significant difference between infiltration rates on alluvial versus upland soils in the Andean study area. The other exception was the significant difference between infiltration rates in topographic coves compared to other slope positions in the tabonuco forest of one watershed in the Luquillo Mountains. Our research provides additional evidence of the ability of forests and forest soils to preserve geomorphic features from denudation by surface erosion, documents the importance of subsurface flow in mountain forests, and supports the need for caution in extrapolating infiltration rates.     

南天山西段古生代火山岩Ar-Ar年龄新资料

根据新近采自中国南天山西段志留-泥盆系乌帕塔尔坎群中的安山岩样品和石炭-二叠纪康克林组上部英安岩角砾样品的全岩Ar-Ar定年测试,乌帕塔尔坎群安山岩的坪年龄为427.70±0.60 Ma,等时年龄为426.96±4.57 Ma; 康克林组上部的英安岩角砾的坪年龄为288.16±0.40 Ma,等时年龄为289.18±2.02 Ma.测试结果为研究中国南天山(西段)古生代造山带的构造体系提供了新的依据.     

六枝煤矿区构造体系初步分析

六枝煤矿区属于威宁—郎岱褶皱束的一部分，NW向构造占据主要地位。地史上该区有多次升降运动，二叠纪的东吴运动，伴随基性岩浆活动；侏罗、白垩纪的燕山运动，使本区发生大规模的褶皱和断裂；喜马拉雅运动的影响使本区构造复杂化。形成NE向扭性断层；构造复合的基本方式是横跨和限制。构造分析表明，NE向构造形成较早，NW向构造形成较晚。     

灵山岩体演化特征及其与稀有金属的成矿关系

从岩体时空分布、岩石化学成分、造岩矿物、副矿物、微量元素、稳定同位素、成岩温度、压力等特征，论述了灵山岩体演化与钽铌等稀有金属成矿的关系，简述了区内典型稀有金属矿床主要成矿地质特征及其与岩体的成因联系，进而肯定了区内钽铌等稀有金属找矿的良好前景，并提出了今后找矿的方向和建议。     

蚕庄金矿上庄矿区控矿构造特征及构造模拟

上庄矿区的主要控矿断裂具有多期活动的特点，主断裂、次级断裂及节理的多种组合方式控制了矿体的产出。运用断裂面波形模拟方法得出了控矿主断裂在成矿期的断裂面波形图，并以此对上庄矿区的深部矿体进行了预测。     

泌阳凹陷北部斜坡带构造特征及油气圈闭有效性

泌阳凹陷北部斜坡带断裂极为发育，主要发育NE向和NWW向两组正断层。NE向断层断距大，延伸距离远；NWW向断层断距相对较小，延伸较短。斜坡带由于构造破碎，断层发育，圈闭类型多为断块、断鼻及断层 岩性复合型圈闭。因此，对北部斜坡带断层的展布和交切规律的研究，是识别该区圈闭的关键。     

山东蒙阴县埠洼金矿与韧性剪切带的关系

埠洼金矿受NW向台上-盘东沟韧性剪切带的控制，矿体产于剪切带中南部的英云质超糜岩中，矿体呈右行侧列式分布，成矿体用与韧性剪切变形变质导致的动力分异作用密切相关，赋矿空间为韧-脆性剪切作用形成的扩容带，是在韧性剪切基础上形成的金矿床。     

辽宁地区的幔枝构造

将辽宁地区划分为4个幔枝构造:山海关幔枝、辽东南幔枝、建平-阜新幔枝、西丰幔枝,文章分述了它们各自组成与构造特点,并举例说明了辽宁幔枝构造通过其三个次级构造单元对成矿的控制规律.     

吉林省水资源可持续利用研究

选取吉林省9城市具有代表性的7项指标,对吉林省水资源可持续利用情况进行了定量分析,采用因子分析(FA)法筛选出3个主因子——水污染排放、水环境质量和水资源,并采用层次分析(AHP)法对3个主因子的协调程度进行了可持续性评价.在分析评价的基础上,对吉林省各城市的水资源可持续利用提出了建议.