拉萨地块南缘热液金铜矿床成矿时代的裂变径迹研究

通过对娘古处、洞嘎和甲马3个矿区计11个磷灰石和锆石裂变径迹年龄分析表明,全区主要有3个成矿期,具体年代约分别为30～40Ma,16～28Ma和11～14Ma,这与区域构造活动期相符.成矿温度均低于锆石裂变径迹退火带的底界温度(～320℃),亦说明陆-陆碰撞以来的构造热事件温度均未超过～320℃.     

试论渭河裂谷成因机制及其意义

渭河裂谷(或渭河地堑)是鄂尔多斯地块南侧的新生代断陷带。本文通过对该区中生代以来区域构造应力-应变场的分析并结合力学分析,认为渭河地区在中生代时,是在由南向北的侧向挤压力作用下形成的一个大型隆起带,且因岩石圈的向上拱起带动了软流圈物质的上涌,从而为新生代裂谷的形成奠定了基础,且对其北侧邻区中生代聚煤作用有明显的控制作用。     

An in situ zircon Hf isotopic,U-Pb age and trace element study of banded granulite xenolith from Hannuoba basalt： Tracking the early evolution of the lower crust in the North China craton

Backscattered electron images, in situ Hf isotopes, U-Pb ages and trace elements of zircons in a banded granulite xenolith from Hannuoba basalt have been studied. The results show that the banded granulite is a sample derived from the early lower crust of the North China craton. It is difficult to explain the petrogenesis of the xenolith with a single process. Abundant information on several processes, however, is contained in the granulite. These processes in-clude the addition of mantle material, crustal remelting, metamorphic differentiation and the delamination of early lower crust. About 80% of zircons studied yield ages of 1842 ±40 Ma, except few ages of 3097-2824 Ma and 2489-2447 Ma. The zircons with ages older than 2447 Ma have high εHf (up to +18.3) and high Hf model age (2.5-2.6 Ga), indicating that the primitive materials of the granulite were derived mainly from a depleted mantle source in late Archean. Most εhf of the zircons with early Proterozoic U-Pb age vary around zero, but two have     

Geochronology of source materials from high-pressure and ultrahigh-pressure metamorphic rocks in Jurassic sedimentary rocks of Hefei Basin

Eclogite cobbles were discovered by Wang et al. (2001) in the Fenghuangtai Formation of the northern margin of Dabie Mountains in the Dushan area of Anhui Province, China[1]. They proposed that after the formation during the Triassic, the high-pressure (HP) and ultra-high-pressure (UHP) metamorphic rocks reached the sur-face through exhumation and uplifting before the late Ju-rassic. However, they have not provided any evidence about isotopic ages. One kind of cobbles of HP-UHP rocks w…     

作物遭受雹灾咋补救?

棉花棉花具有很强的生理补偿作用和再生能力,遭受雹灾后,只要加强管理,仍能获得较好收成,不要轻易翻种.①中耕松土.及早进行中耕、晾墒,以增温通气,控制死苗,促进早发;特别是盐碱地棉田,更应及时松土,防止返盐死苗.②追施速效氮肥.一般地块,每亩可追施尿素5～7.5千克或碳铵13～15千克.追肥时,肥料要距离棉株10～13厘米,以防烧根.③及时治虫.棉株受灾后萌发的枝叶较为幼嫩,前期蚜虫多,后期易受棉铃虫、棉小造桥虫等危害,要早治、狠治,做到每叶必保,每蕾(铃)必争.必要时,可在棉株萌芽初期喷药防治蚜虫.④科学整枝.     

浅谈城市地块的开发与建设策略

城市化发展进程的速度越来越块,土地作为不可再生资源越来越紧缺,因此在房地产规划中高密度住宅小区越来越多。本文就针对某地块居住项目规划设计方案进行分析,解读其规划设计以及建筑设计的具体过程与实施原则。     

关于苏南地区开发区市政工程规划建设的几点思考

本文从开发区路网规划建设的角度入手,研究路网的布局、路幅宽度布置的选择、开发区水系的分析、道路标高的控制以及地块填高的控制,研究如何打造一个经济、合理、美观且运行良好的经济开发区。     

狭长地块的别墅规划设计探讨——铁岭新天地别墅区项目的规划设计过程回顾

本文笔者运用常规别墅区规划设计的方法,针对项目中地形狭长的特点,以具体工程为依据,阐述了狭长地块别墅规划设计中需要考虑的问题。     

巴彦浩特盆地构造特征及含油气远景初步评价

巴彦浩特盆地是-个上叠于阿拉善地块之上的复合盆地．盆地可划分成五个-级构造单元,十二个次-级构造单元。盆地中发育有五种构造地层组合．断裂对盆的形成和发育起明显的控制作用,巴彦乌拉山断裂为-深切基底的铲地正断层,该断裂控出了西部拗陷带的形成,其活动强度自北向南减弱．伊南断裂带控制了伊和凹陷的形成,该断裂带中段活动强度最大;查汗断裂具明显的左旋走滑特征。盆地中发育多种构造样式,主要有：叠瓦状冲断层、滚板构造、牵引褶皱、铲形正断层、滚动背斜、“垒-堑”构造等。石炭系是盆地内主要的生油层系,它广泛发育并具良好圈闭条件的东部地区和南部地区有较好的油气远景。