P-T path determinations in the Tormes Gneissic Dome, NW Iberian Massif, Spain

The Tormes Gneissic Dome (TGD, NW sector of the Iberian Massif, Spain) is a high-grade metamorphic complex affected by a major episode of extensional deformation (D2). The syn-D2 P–T  path of the Lower Unit of the TGD was deduced from the analysis of reaction textures related to superimposed fabrics developed during exhumation, analysis of mineral zoning and thermobarometric calculations. It comprises an initial phase of decompression, determined using the tweequ thermobarometric technique, from 6.4–8.1 kbar at 735–750 °C (upper structural levels) and 7.2 kbar at 770 °C (lower structural levels) to 3.3–3.9 kbar and 645–680 °C. This evolution is consistent with the observed sequence of melting reactions and the generation of garnet- and cordierite-bearing anatectic granitoids. The later part of the syn-D2 P–T  path consisted of almost isobaric cooling associated with the thermal re-equilibration of the unit in the new structural position. This segment of the P–T  path is recorded by assemblages with And +Bt+Ms and Ms+ Chl +Ab related to the later mylonitic S2 fabrics, which indicate retrogression to low-amphibolite and greenschist facies conditions.     

遥感影像用于城市扩展监测的研究

通过焦作市城市扩展监测的实践,对以多时相遥感影像监测城市扩展进行了研究,阐述了以地形图及TM遥感影像为数据源,利用RS和GIS软件进行图像处理,提取城区扩展的变化信息,并对其扩张变化的主要方向、速度及规律进行监测和分析;论述了交通建设、政策法规、经济投资区的建设和当地的自然地理环境对城市的扩展速度和方向的影响。     

焦家构造带控矿作用探讨——以莱州新城金矿床为例

概略陈述了新城金矿床及焦家构造带的基本地质特征.对焦家构造带成矿前后的构造应力场、矿体侧伏规律、NWW向矿化带的形成及成矿时代等问题进行了探索性讨论.     

哈长城市群城镇用地扩展进程及其驱动因素研究

以Landsat TM/ETM+/OLI遥感影像为主要数据源,提取哈长城市群1990、2000、2010、2015 年4 个年份的建设用地信息,采用年均扩展指数、景观扩展指数、多距离空间聚类函数、空间分维度等对城镇用地扩展进程进行分析。结果表明,1990~2015年间,哈长城市群城镇用地增加57 321.47 hm²,增长率为21.05%,整体扩展强度呈上升趋势;空间扩展表现出以中心城市为核心的扩展模式,边缘式增长在各个时期均为主导增长方式;空间扩展聚集性总体表现出“先增强、后减弱”趋势,整体空间结构相对稳定。国家宏观政策、非农业GDP增量和第三产业GDP增量是影响哈长城市群城镇用地扩展的重要因素。GDP增量、非农业人口增量、第二产业GDP增量对城镇用地的扩展起阶段性作用;人均GDP增量与城市用地扩展相关性不显著。     

Climate advice and extension practice

This article unpacks the problematic relationship between emerging climate change adaptation norms and changes underway in agricultural extension. It is increasingly recognised that in order to apply new knowledge about climate change in rural development practice a more institutional perspective is needed, but there is no clear consensus on what this implies. This article looks at agricultural extension as an example of a meso-level institution that is frequently assumed to be a major potential “implementing partner” in climate adaptation efforts, at the same time as it is also often portrayed as a worst-case example of the obstacles encountered in changing the focus of a path dependent bureaucracy. This article contrasts the perspectives of normative climate adaptation frameworks (exemplified by the 2011 World Resources Report) with what is known about prevailing extension trends and realities. It is suggested that long lists of recommended climate adaptation tasks and technologies may distract from an understanding of the institutional change processes underway within meso-level institutions, wherein the climate agenda would need to be merged with other agendas related to pluralistic, pragmatic, accountable, sustainable and market-oriented rural development.     

Drainage integration and sediment dispersal in active continental rifts: A numerical modelling study of the central Italian Apennines

Progressive integration of drainage networks during active crustal extension is observed in continental areas around the globe. This phenomenon is often explained in terms of headward erosion, controlled by the distance to an external base‐level (e.g. the coast). However, conclusive field evidence for the mechanism(s) driving integration is commonly absent as drainage integration events are generally followed by strong erosion. Based on a numerical modelling study of the actively extending central Italian Apennines, we show that overspill mechanisms (basin overfilling and lake overspill) are more likely mechanisms for driving drainage integration in extensional settings and that the balance between sediment supply vs. accommodation creation in fault‐bounded basins is of key importance. In this area drainage integration is evidenced by lake disappearance since the early Pleistocene and the transition from internal (endorheic) to external drainage, i.e. connected to the coast. Using field observations from the central Apennines, we constrain normal faulting and regional surface uplift within the surface process model CASCADE (Braun & Sambridge, 1997, Basin Research, 9, 27) and demonstrate the phenomenon of drainage integration, showing how it leads to the gradual disappearance of lakes and the transition to an interconnected fluvial transport system over time. Our model results show that, in the central Apennines, the relief generated through both regional uplift and fault‐block uplift produces sufficient sediment to fill the extensional basins, enabling overspill and individual basins to eventually become fluvially connected. We discuss field observations that support our findings and throw new light upon previously published interpretations of landscape evolution in this area. We also evaluate the implications of drainage integration for topographic development, regional sediment dispersal and offshore sediment supply. Finally, we discuss the applicability of our results to other continental rifts (including those where regional uplift is absent) and the importance of drainage integration for transient landscape evolution.     

小城镇空间结构变迁的形式和动力

小城镇向心增长的空间过程主要表现为郊区城镇化、内城更新改造、反向扩展3种形式，是小城镇对农村人流、物流的集聚和内部空间结构的优化。小城镇离心增长的空间过程主要表现为城镇郊区化、产业区位变迁、外向扩展3种形式，是小城镇生产力发展到一定阶段后城镇要素向近郊区的扩散。小城镇向心增长和离心增长是集聚与扩散相互作用的表现，社会经济发展是小城镇空间变迁的根本动力，功能－形态互适机制是其演变的主要机制。     

区域城市化水平的物元可拓综合评判——以福建省为例

在建立区域城市化水平评价指标体系的基础上,运用物元可拓方法和主成分分析方法,以福建省23个主要城市为研究地域单元,建立了福建省区域城市化水平综合评判模型.模型的输出结果表明,福建省区域城市化水平总体偏低,各地区在发展水平上出现明显分层;模型的综合关联度将福建省区域城市化水平划分成4个等级,分项指标关联度则揭示了各地区城市化发展的薄弱环节.研究结果较为客观地反映了福建省城市化的实际状况,为区域城市化水平的评价提供了一种新的研究思路.