据了解，本次比赛项目为公开组22人龙舟500米直道竞速，共有12支国标龙舟队参赛，汉寿县内组织4支，县外邀请8支。县外邀请的8支队伍分别是2019年全国第十一届少数民族传统体育运动会龙舟赛冠军麻阳县龙舟队、汩罗江龙舟大赛冠军汨罗市双楚龙舟队、2024年湘阴县洋沙湖民俗龙舟赛冠军湘阴县龙舟队、2024年长沙千龙湖暨望城端午文化节龙舟邀请赛200米冠军浏阳河青年龙舟队、2024年陕西商洛公开赛冠军娄底市双峰龙舟队、2024年长沙千龙湖暨望城端午文化节龙舟邀请赛500米冠军长沙市花桥龙舟队、桃江县龙舟赛冠军桃江县武潭龙舟队、2024年娄底首届龙舟争霸赛500米冠军新化县新龙爪龙舟队；汉寿县的四支队伍分别是2009年贵州铜仁全国传统龙舟大赛冠军汉寿县新力量龙舟队、2024年中国辉煌足迹—柳叶湖龙舟公开赛大众组200米、500米双料冠军湖南高旅职院龙舟队、2024年柳叶湖龙舟赛500米冠军汉寿县特工队龙舟队、2024年汉寿县清水湖杯传统龙舟赛冠军汉寿县圣元红龙舟队。
2025年01月07日，3. 江西瑶里古镇
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桑葚干的铁含量是水果类中最高的每100驳含铁42.5尘驳是名副其实的补血名副其实的补血果将桑葚干煮粥吃不但可以补血还可以美容
吉他也可以自制，虽然没有自由，但也阻挡不了心中的音乐梦。测绘学报 | 王帅：利用空间大地测量资料研究大陆区域构造变形模式2021-08-25 11:29·测绘学报本文内容来源于《测绘学报》2021年第6期（审图号GS（2021）3565号）利用空间大地测量资料研究大陆区域构造变形模式王帅南京工业大学测绘科学与技术学院, 江苏 南京 211816引文格式：王帅. 利用空间大地测量资料研究大陆区域构造变形模式[J]. 测绘学报，2021，50(6)：852-852. DOI: 10.11947/j.AGCS.2021.20200323WANG Shuai. Study on the crustal deformation pattern in continental regions using the space geodesy[J]. Acta Geodaetica et Cartographica Sinica, 2021, 50(6): 852-852. DOI: 10.11947/j.AGCS.2021.20200323：http://xb.sinomaps.com/article/2021/1001-1595/2021-6-852.htm博士论文摘要地壳运动与变形模式受岩石圈深浅部结构、构造单元边界动力和深部动力、断裂带几何和运动特性等多种因素影响。本文以空间大地测量观测技术为手段，综合区域断层活动性、地形地貌特点、岩石圈结构属性和历史地震目录等资料，对帕米尔高原东西向剪切变形、苏拉威西拉张变形和巴布亚新几内亚逆冲汇聚变形进行了研究，相关研究对认识大陆动力学和地震动力学等具有重要的意义。研究内容主要包括：(1) 帕米尔高原东西向剪切变形模式。在印度板块和欧亚板块碰撞挤压作用下，帕米尔高原以北部弧形构造带的南北向缩短为主，同时，沿木吉-公格尔断裂带，高原还呈现出显著的东西向剪切变形。利用GNSS和InSAR观测资料分析了帕米尔高原地壳运动特征，着重分析了高原东西向剪切变形特征；同时，结合历史地震目录和区域强震震源机制，对木吉-公格尔断裂在高原剪切变形过程中扮演的角色进行了分析；并讨论了高原剪切变形的动力学机制。结果表明：①木吉-公格尔断裂带是一条剪切变形带，其东部地壳向东运动，西部地壳向西运动，表现为木吉断层的右旋剪切变形和公格尔断裂的东西向拉张剪切变形；②木吉-公格尔断裂带是帕米尔高原与塔里木盆地之间的构造边界带，吸收和调节着两者之间的相对变形；③帕米尔高原剪切变形是下地壳熔融层内的韧性流动在地表的力学响应。(2) 苏拉威西中部拉张构造变形模式。苏拉威西位于印度尼西亚东部，吸收并调节着澳大利亚板块、巽他板块和菲律宾板块之间的汇聚变形，构造运动复杂，火山活跃，地震频发且类型多样。帕卢—科罗走滑断层从南向北贯穿苏拉威西中部，是区内一条重要的大型左旋走滑断裂带，且以其为边界断裂的东苏拉威西中部块体表现为明显的拉张应变。基于区域断层活动性、地形地貌资料和历史地震目录提出了“漏斗”运动学模型，用于解释苏拉威西中部地壳的拉张变形及其演化过程。研究表明：①苏拉威西中部地壳运动分为造山阶段和物质挤出阶段两个阶段。两个阶段都涉及物质的积累和挤出，第1个阶段物质的积累占主导，第2个阶段物质的侧向挤出占主导；②沿帕卢—科罗断裂带的物质侧向挤出作用促进了苏拉威西的重力滑塌，导致了该区域地壳的拉张与减薄。(3) 巴布亚新几内亚逆冲褶皱带变形模式。巴布亚新几内亚位于澳大利亚板块和太平洋板块碰撞的前缘地带，区内逆冲褶皱带普遍发育。基于InSAR观测资料对2018年巴布亚新几内亚Mw 7.5地震的同震形变进行了分析；确定了此次地震的多断层破裂模型，并对同震滑动分布特征进行了反演。结合地形地貌资料、岩石圈结构特性、反演确定的构造几何及滑动分布模型对逆冲褶皱带地壳增厚机制与应变积累方式进行了讨论。结果表明：①2018年巴布亚新几内亚Mw 7.5地震是一个多断层破裂事件，共涉及了4个断层的破裂，以基底逆冲为主，破裂深度超过了25 km；②逆冲褶皱带沿走向变化的地形地貌特点与岩石圈属性和构造几何有关，西段岩石圈温度较低，强度较大，东段岩石圈温度较高，强度较弱；西段的断裂倾角要比东段的陡；③巴布亚新几内亚逆冲褶皱带上地壳的增厚隆升可能受控于基底断层的运动。作者介绍第一作者介绍：王帅(1988—), 男, 2019年6月毕业于武汉大学, 获工学博士学位(指导教师: 许才军教授), 研究方向为地壳形变监测。E-mail: shwang@njtech.edu.cn初审：张艳玲复审：宋启凡终审：金 君
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但我觉得小两口每月有15000的收入还4000房贷不是问题也就没管
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