Zircon U-Pb SHRIMP dating for the volcanic rocks of the Xiong’er Group: Constraints on the initial formation age of the cover of the North China Craton

The volcanic rocks of the Xiong‘er Group occur widely in the southern part of the North China Craton, which mark the beginning of the cover in the southern part of the North China Craton. The age of the volcanic rocks is thus crucial to understand the tectonic regime and evolutionary history of the North China Craton in the Proterozoic age. Zircons from five volcanic rocks and intrusions were dated by U-Pb SHRIMP method. The results indicate that the Xiong‘er Group formed in 1.80--1.75 Ga of Paleo-Proterozoic. Since the Xiong‘er Group formed earlier than the Changcheng System, the earliest rocks in the Changcheng System is therefore assumed to be formed in 1.75 Ga. A thermal-tectonic event of ca. 1.84 Ga is indicated by new zircon U-Pb SHRIMP ages in the southern part of the North China Craton. The volcanic rocks of the Xiong‘er Group thus represent the initial magmatism of the Paleo-Proterozoic breakup of the North China Craton. Numerous inherited zircons in the volcanic rocks mainly formed in ～2.20 Ga, indicating that the source magma of the volcanic rocks may be derived from the ～2.20 Ga crust, or from a mantle magma with significant contamination of the ～2.20 Ga crust.     

不完全区组设计与测地块的构造

我们只讨论有限、无向、简单图。 设图G连通,如果对G中任二点x,y,x到y的最短路均唯一,则称G为测地图。如果G是二连通的测地图,则称G为测地块。 测地块的构造问题是测地图的研究中一个十分重要而又相当困难的问题。在这方面,     

最大值原理在地块价格评价中的应用

应用Pontryagin 最大值原理,讨论了在一般的权函数下对地块上建筑物的最优维修投资计划以及地块价格的评价问题.     

Permian volcanisms in eastern and southeastern margins of the Jiamusi Massif, northeastern China: zircon U-Pb chronology, geochemistry and its tectonic implications

LA-ICP-MS zircon U-Pb dating and geochemical data for the Late Paleozoic volcanic rocks from eastern and southeastern margins of the Jiamusi Massif are presented to understand the regional tectonic evolution. Zircons from eight representative volcanic rocks are euhedral-subhedral in shape and display striped absorption and fine-scale oscillatory growth zoning as well as high Th/U ratios （0.33-2.37）, implying a magmatic origin. The dating results show that the Late Paleozoic volcanic rocks in the study area can be divided into two stages, i.e., the Early Permian （a weighted mean 205^Pb/238^U age of 288 Ma） and the Middle Permian volcanisms （a weighted mean 205^Pb/238^U age of 268 Ma）. The former is composed mainly of basalt, basaltic-andesite, andesite and minor dacite. They are characterized by low SiO2 contents, high Mg^# （0.40-0.59）, enrichment in Na （Na2O/K2O = 1.26-4.25） and light rare earth elements （LREEs）, relative depletion in heavy rare earth elements （HREEs） and high field strength elements （HFSEs）, indicating that an active continental margin setting could exist in the eastern margin of the Jiamusi Massif in the Early Permian. The latter consists mainly of rhyolite and minor dacite with high SiO2 （77.23%-77.52%）, low MgO （0.11%-0.14%）, enrichment in 1（20 （Na2O/K2O ratios 〈 0.80） and Rb, Th, U and depletion in Eu, Sr, P and Ti, implying a crust-derived origin. Therefore, it is proposed that the Middle Permian volcanic rocks could have formed under the collision of the Jiamusi and the Khanka Massifs.     

青藏高原东部及邻区地块现今运动特征

青藏高原东部及邻区为典型的大陆地壳变形区.根据GPS监测结果,得出了欧亚参考框架的运动速度场;采用刚性假设下最小二乘法,对地块现今运动进行了研究.GPS监测结果表明:柴达木地块、甘青地块、华南地块、川滇地块、印支地块运动速率分别为(11.95士2.89)mm/a,(11.86士2.32)mm/a,(7.83士2.08)mm/a,(13.18±2.43)mm/a,(6.45士1.95)mm/a;运动方向分别为61.1°,93.8°,113.1°,134.8°,141.6°;旋转速率分别为2.91×10-9rad/a,6.91×10-9rad/a,0.38×10-9rad/a,2.15×10-9rad/a,1.45×10-9rad/a.柴达木地块、甘青地块、川滇地块活动性较强,而华南地块、印支地块活动性较弱,属于稳定地块;各块体围绕东喜马拉雅构造结呈顺时针旋转.地块规律性运动特征与印度板块向北俯冲、推挤有作密切关系;而地块的差异运动则与总体构造应力条件下远程边缘效应及地块之间相互作用有关.     

基于GF-1 PMS的玉米出苗情况提取

及时、准确的玉米出苗情况监测可以为农田经营管理和宏观决策提供玉米出苗期的生长信息,便于及时采取适当的科学管理措施,达到增产增收的目的。归一化植被指数（Normalized Difference Vegetation Index, NDVI）及与作物生长状态关系密切,可以用于评价玉米的出苗情况。采用地块的NDVI均值及均方差可以反映地块内玉米出苗的综合情况,以吉林省长春市九台市榆树村和解放村为例,对研究区玉米出苗情况信息进行提取,最后利用实地采集的验证数据对提取结果进行验证。研究区玉米出苗情况信息提取结果的总体精度达到80%,表明利用上述方法能够在一定程度上反映玉米的出苗情况,可以为玉米出苗情况评价提供参考依据。     

新疆阿拉塔格地区新元古代花岗片麻岩的锆石U-Pb定年与Hf同位素: 对中天山地块前寒武纪地壳演化的制约简

中天山地块前寒武纪结晶基底的组成和形成历史,是揭示天山造山带构造演化的关键问题. 本文对分布在中天山地块阿拉塔格地区的花岗片麻岩进行了LA-ICP-MS锆石U-Pb年代学和LA-MC-ICPMS锆石Hf同位素研究. 两个研究样品中的岩浆结晶锆石分别获得了945±6和942±6 Ma的原岩形成年龄,揭示了阿拉塔格地区存在新元古代早期的岩浆活动. 这些岩浆结晶锆石的Hf模式年龄远大于其结晶年龄,分别为1.82~2.22和1.70~2.03 Ga,反映了它们的岩浆均起源于古老地壳的再造. 但是这一古元古代的Hf模式年龄很可能是新元古代地壳中不同时代古老地壳物质混合的结果. 在这两个花岗片麻岩中还获得了989~1617 Ma的继承碎屑锆石年龄,它们具有变化较大的锆石Hf同位素组成,模式年龄为1.54~2.30 Ga,且部分1.4~1.6 Ga锆石具有接近亏损地幔的¹⁷⁶Hf/¹⁷⁷Hf初始值,反映了中元古代时期在中天山地块存在新生地壳形成和古老地壳再造事件,显示出与塔里木克拉通显著不同的前寒武纪地壳形成和演化历史. 中天山地块的前寒武纪地壳基底可能并不是来自塔里木克拉通的一部分.     

干热河谷区土地整理对种植业经济效益的影响

经济效益是土地整理的主要目标，辨析土地整理对项目区种植业经济效益的影响，对于土地整理项目前期工程设计和后期农业生产管理意义重大。在中国西南区干热河谷地带选取已竣工多年并且种植业生产相对稳定的典型土地整理项目区，通过田间调查走访获取一手资料，运用统计方法进行数据处理。调查结果显示，土地整理项目区目前主要发展果品生产，葡萄种植面积占比达到80%以上，葡萄单位面积净利润显著超过传统作物柑橘和玉米，每公顷分别高出11.43万元和19.38万元，并且葡萄优良新品种单位面积净利润显著高于常规品种；葡萄种植近3年间经济效益保持稳定，在地块由小到大的变化过程中，单位面积净利润先升后骤降再回升，并保持适度稳定。研究发现，土地整理促使种植业结构发生根本改变，农业生产经济效益显著增加；在土地整理项目设计和施工中应尽可能构建大面积地块；在农业生产管理中应及时将主导作物更新为优良新品种。