南四湖周边地区第四纪地层划分的初步研究     

张祖陆  孙庆义  宋印胜  王梅 《山东国土资源》2007,23(6):2007/3/14-2007/6/22

依据南四湖周边地区数十眼钻孔的数据资料，以岩性地层分析对比研究为基础，通过利用“C、热释光等年代测定和孢粉分析技术方法，对该地区第四纪地层的划分提出了初步认识。经研究认为，该区中南部的南四湖、北五湖的湖相沉积大约形成于全新世中晚期之后。根据区内松散岩层的沉积物岩性和岩层的组合特征可以划分出5个岩组段。  相似文献   

土地利用规划环境影响评价中不确定性分析   总被引：2，自引：0，他引：2  

刘晓丽 《山东国土资源》2007,23(9):28-30,33

在分析土地利用规划环境影响评价中的不确定来源、特点及其对决策的影响基础上,提出了降低环境影响评价中不确定性的方法。通过研究认为:土地利用规划环境影响评价中的不确定主要由土地利用规划方案的不确定、环境信息的不确定和环境影响程度的不确定引起的,这些不确定性具有客观性、传递性、累积性,对决策会产生较大的干扰,但是可以通过使用基于情景分析的预测方法、多方协作的方式以及广泛开展公众参与等方法来降低。  相似文献   

Geomorphological records of a ‘flood-dominated regime’ in the Rhône Delta (France) between the 1st century BC and the 2nd century AD. What correlations with the catchment paleohydrology?     

《Geodinamica Acta》2002,15(1):79-92

In the Rhône Delta, numerous paleoenvironmental indicators coming from geomorphology, sedimentology, paleoecology and archeology provide evidences of remarkable hydrological regime change at the beginning of the Roman Antiquity. A significant reinforcement in the Rhône Riverˈs competence is indicated by the increase in grain size of the sediments deposited in the floodplain, within the immediate proximity of the channel. Increase in the fluvial sediment yield is indicated by the increase in rate of sedimentation in the floodplain. Increase in water levels is indicated by the deposition of hydromorphous facies, the development of hydrophytic species, and the decrease in activity of terrestrial lombricoids in the floodplain. Numerous crevasse splays were formed by short-term avulsions of the Rhône River between the first century BC and the AD first century. Their frequency is related to an increase of Rhône River paleodischarge, which makes the channel network incapable of evacuating large volumes of water brought in by the river. The littoral zone experienced a phase of progradation between the AD 1st and the 3rd centuries, in relation to the increase of terrigenous deposits coming from the Rhône of Ulmet. The increase in solid discharge, in the flood-dominated regime (FDR) context, can be related to the overall increase in detrital output from the catchment. The Rhône Delta rather appears in phase with the northern Alps and Massif Central from the 1st century BC to the AD 1st century. The FDR at the beginning of the Christian era contrasts with the drought-dominated regime (DDR) and the reduction of torrential rainfall in the Mediterranean and south Alpine areas. These observations allow to confirm the hydroclimatic limit which could distinguish the southern part of the catchment (Provence, Durancian Alps) from the rest of the Rhône basin.  相似文献   

利用层次分析法评价东营市浅层地热能适宜性          下载免费PDF全文

胡松涛  孙云川  胡思敬 《山东国土资源》2014,30(7):42-45

利用定性、半定量相结合的层次分析法(AHP),建立地埋管换热系统适宜性递阶层次结构模型,在野外试验、室内测试等基础数据的基础上,选取地下水埋藏深度、砂层厚度、成孔难易程度、地面沉降、热扩散率、比热容、综合热导率等7个评价指标,将东营市浅层地热能开发利用划分为适宜区、较适宜区。这是东营地区第一次利用实测数据开展浅层地热能适宜性评价,为今后的合理开发利用提供了科学依据。  相似文献   

十堰至天水高速公路磨河村隧道工程地质条件分析          下载免费PDF全文

王涛  张海林 《山东国土资源》2014,30(7):37-41

通过对隧址区地形地貌、地层岩性、地质构造、岩土体工程地质特征等的调查,结合工程物探、地质钻探,岩体物理力学试验和地质测绘等勘察成果,分析了隧道洞身及进出口处围岩的稳定性,指出隧道施工过程中可能会遇到的工程地质问题,并提出了超前地质预报、支护、预防地质灾害、保护生态环境等施工措施和建议。  相似文献   

山东省构造型地裂缝成因机制研究          下载免费PDF全文

安海波  王宝春  张长龙 《山东国土资源》2014,30(2):34-37,42

收集了山东省多年来的地裂缝地质灾害调查和研究资料,结合地裂缝地质灾害发育的地质环境背景,对山东省内地裂缝的区域分布特征、发育特点进行了分析,认为山东省内构造型地裂缝广泛发育,并对山东省构造型地裂缝的成因机理进行阐述。  相似文献   

3 D inversion of borehole gravity data using cokriging          下载免费PDF全文

GENG Meixia  HUANG Danian  XU Bowen 《世界地质(英文版)》2014,17(4):225-230

Borehole gravity has been used in mineral exPloration recently with the advent of slim-hole gravime-ters. It is logical to Perform inversion to utilize the information in the newly acquired data. The i...  相似文献   

近10年来山东省城镇化水平时空差异分析     

赵明华  包维虎  韩荣青 《世界地理研究》2014,(4):97-106

运用泰尔指数和标准差系数,测度2000年~2012年山东省城镇化水平的总体和省内东中西三大区域及其内部差异。结果表明:(1)山东省城镇化水平总体差异在2009年之前总体上呈现扩大趋势,2009年之后差异开始减小;(2)东、中、西部之间的差异总体上呈现波动上升的趋势,中部内部的差异相比东部和西部更明显;(3)2010年之前三大区域内部差异对总体差异的贡献率占主导,2010年之后三大区域之间差异对总体的贡献率占据主导地位;(4)通过分析近十年影响山东省城镇化水平差异变动的因素得出,经济发展水平、产业结构以及区位条件是造成差异的主要原因。因此,山东省城镇化未来的发展应该着力促进产业结构的优化升级,尤其是第三产业的发展,其次促进各地区之间的联系,坚持"一圈一区一带"的发展战略,促进各个地区的城镇化水平的协调发展,缩小差异,最终实现区域城镇可持续发展。  相似文献   

Postdated melting of subcontinental lithospheric mantle by the Emeishan mantle plume: Evidence from the Anyi intrusion,Yunnan, SW China     

《Ore Geology Reviews》2014

The Anyi intrusion is located in the central zone of Emeishan large igneous province (ELIP), SW China. It outcrops in an area of about 0.65 km² and ~ 1 km thick and dips to the southwest. The Anyi intrusion consists of a lower clinopyroxenite zone, middle gabbro zone, and an upper monzonite–syenite zone. Up to 400 m thick stratiform disseminated Fe–Ti oxide layer with grades of 16–18 wt.% total Fe is hosted in the lower clinopyroxenite zone. Zircon SHRIMP U–Pb age (247 ± 3 Ma) indicates that the Anyi intrusion represents postdated mafic magmatism resulting from the ~ 260 Ma Emeishan mantle plume. Compared with the typical oxide-bearing intrusions (such as Panzhihua and Baima) formed at ~ 260 Ma in the ELIP, the Anyi intrusion is characterized by high alkaline contents and LREE/HREE ratios, extremely low εNd values (− 6.2 to − 7.6) and moderate high (⁸⁷Sr/⁸⁶Sr)_i values (0.7072 to 0.7086). These characteristics of the Anyi intrusion cannot be explained by fractional crystallization or crustal contamination, but may reflect a unique enriched continental lithospheric mantle source (a mantle source mixed between garnet pyroxenite and spinel peridotite). We propose that the postdated mafic magmatism associated with the formation of the Anyi intrusion and its Fe–Ti oxide ore may be the product of melting of a mantle source mixed between garnet pyroxenite and spinel peridotite in the shallow lithosphere caused by conductive heating combined with lithosphere thinning due to plume–lithosphere interaction.  相似文献   

山东张家洼矽卡岩型铁矿矿物学特征及其对成矿环境的指示意义          下载免费PDF全文

费详惠  张招崇韩 鎏 《中国地质》2014,41(6):1873-1896

张家洼矽卡岩型铁矿位于华北克拉通东南部,赋存在石炭系本溪组与奥陶系马家沟组之间的假整合面处及闪长岩体与奥陶系马家沟组大理岩的接触带附近,富铁矿石资源量已达大型规模。研究发现矽卡岩矿物种类在内外接触带分布有一定区别,内带为石榴石等钙质矽卡岩矿物,而外带为阳起石、金云母等镁质矽卡岩矿物,整体构成钙镁质矽卡岩。对矽卡岩矿物系统的研究表明,透辉石及石榴石发育有环带,其氧化物含量随矿物环带的形成比例不断变化,暗示酸碱度及氧逸度随着成矿流体的演化而发生相应的变化,即由早期矽卡岩阶段的相对还原的酸性环境演化为退化蚀变阶段相对氧化的碱性环境从而导致铁质逐渐萃取多次富集、沉淀,后期随着磁铁矿的沉淀又逐渐在硫化物阶段转化为还原环境生成金属硫化物。  相似文献