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1.
Granitoid gravels are discovered from alluvial fan conglomerates, the base of Jurassic Fenghuangtai Formation (J2 2), in the north margin of Dabie block and the south part of the Hefei Basin. These granitoid gravels make up 5%–10% of all gravels by volume percent. For the four components, K-feldspar, biotite, amphibole and whole rock divided from two selected granitoid gravel samples, their Rb-Sr isotopes are measured, which gives two formation ages of granitoids: (428±20) Ma and (430±54) Ma, and means that the Early Paleozoic granitoid intrusive rocks once existed in the Dabie Mountain provenances of Jurassic. The granitoids occur in the tectonic setting of post-collision uplift according to lithogeochemical discriminant analysis. 相似文献
2.
LI Renwei SANG Haiqing ZHANG Renhu CHU Zhuyin LI Shuangyin JIN Fuquan & JIANG Maosheng . Institute of Geology Geophysics Chinese Academy of Sciences Beijing China . Department of Resource Environment Sciences Hefei Industrial University Hefei China 《科学通报(英文版)》2003,48(6):605-610
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… 相似文献
3.
The nonlinear dynamical behaviors of artificial neural network (ANN) and their application to science and engineering were summarized. The mechanism of two kinds of dynamical processes, i.e. weight dynamics and activation dynamics in neural networks, and the stability of computing in structural analysis and design were stated briefly. It was successfully applied to nonlinear neural network to evaluate the stability of underground stope structure in a gold mine. With the application of BP network, it is proven that the neuro-com-puting is a practical and advanced tool for solving large-scale underground rock engineering problems. 相似文献
4.
The studies of continental deep subduction and ultrahigh-pressure metamorphism have not only promoted the development of solid earth science in China, but also provided an excellent opportunity to advance the plate tectonics theory. In view of the nature of subducted crust, two types of subduction and collision have been respectively recognized in nature. On one hand, the crustal subduction occurs due to underflow of either oceanic crust （Pacific type） or continental crust （Alpine type）. On the other hand, the continental collision proceeds by arc-continent collision （Himalaya-Tibet type） or continent-continent collision （Dabie-Sulu type）. The key issues in the future study of continental dynamics are the chemical changes and differential exhumation in continental deep subduction zones, and the temporal-spatial transition from oceanic subduction to continental subduction. 相似文献
5.
As an important part of the global continents, China continent has long been situated in the peculiar tectonic position and experienced extremely complicated activities, which resulted in the regional unique characteristics for China continent on the global common geological background. These characteristics contain abundant information regarding scientific key issues of modern geological frontier. Thus, China continent can be a natural laboratory and excellent arena for the modern geosciences. The modern earth sciences have started entering the era featured with earth systematic science and beyond plate tectonics. How to take the regional advantage and exploit the treasure resource to participate the new theoretical and methodological creation is a historic opportunity and great challenge we are facing. This paper generalizes research priorities in four fields on China continental geology and tectonics for discussion. They are: China continental tectonics and dynamics; Mesozoic-Cenozoic crustal deformation and deep-seated processes in China continent and the adjacent regions; deep-seated dynamic background and evolutionary trend of crustal tectonic activities on the time scale of human existence; deep-seated background and processes of conjunction and transformation of different tectonic systems. 相似文献
6.
The discovery of granite gravel in Hefei Jurassic backland basin, which came from the Dabie Shan or North Huaiyang, has a great significance for probing into uplift and exhumation of the Dabie orogenic belt. Lithochemical and isotope chronological analyses on the granite gravel in the Sanjianpu Formation and the Fenghuangtai Formation in Jinzhai County prove that post-orogenic granite was developed in the major provenance of the Hefei Basin; that is, Dabie Shan or North Huaiyang. Discordant lower intersection point age of zircon U-Pb of granite gravel is about 214 Ma, and40Ar/39Ar age of muscovite about 196 Ma, K-Ar age of K-spar about 181 Ma. The former is the diagenetic age of the sample, and the latter two represent the sealed ages of muscovite and K-spar respectively. The age of sedimentary rocks in which a lot of granite gravels appear in the sedimentary section may represent the newest age of the exhumation of the granite body, so we assume that the age is 166 Ma. Therefore, we calculated the uplift rates of the granite body from Late Triassic to early Middle Jurassic; that is about 0.08 km/Ma and 0.4–0.3 km/Ma in the early slowly uplifting stage and later fast uplifting stage respectively, after the formation of the body at 214 Ma. These results are basically identical to the uplifting ages of the Dabie ultrahigh pressure metamorphic (UHPM) belt and the North Huaiyang thrust belt. 相似文献
7.
针对强夯机满载率高,起重卸载频繁,工作环境恶劣等特点,以某新型强夯机为研究对象,基于多体系统动力学理论,考虑臂架各部件的柔性,建立了强夯机多体系统刚柔耦合动力学模型,通过动态响应仿真与试验对比,研究了整机在典型工况下的动力学特性,得出了臂架关键部件的运动规律及应力结果。借助于刚柔耦合动力学计算结果,根据优化设计理论和方法建立臂架结构优化的数学模型,通过优化计算后的臂架结构应力减少12.48%,最大位移减少15.47%,臂架总质量减少6.52%,强度得以充分发挥,整机各项性能得以改善。 相似文献
8.
深化大陆构造研究 发展板块构造 促进固体地球科学发展 总被引：4，自引：0，他引：4
目的提出深化大陆构造研究,发展板块构造,推动固体地球科学发展的思考与建议,以引起关注与讨论。方法面对当代地球科学的最新发展和板块构造与大陆动力学研究的新进展,根据中国大陆地质与大陆构造在全球共性中的地域突出特点及其在现代地学发展中的独特意义,提出深化大陆构造研究的思考和建议。结果提出了一系列新的思考和建议。结论深化大陆构造研究是发展板块构造,推动固体地球科学发展的必由之路,势在必行。 相似文献
9.
辽河盆地老第三纪火山岩及其构造环境分析 总被引：5，自引：1，他引：4
认为辽河盆地老第三纪火山岩属玄武岩类,这种玄武岩为碱性系列,每期火山活动的晚期存在碱性玄武岩系列与拉斑玄武岩系列的共生。与渤海湾盆地其他地区一样,它们是在稳定的构造环境,即大陆板内由断裂活动引起的喷发,属典型的大陆裂谷玄武岩。 相似文献
10.
Based on detailed field investigations and petrographic observations, we discovered Neoproterozoic-emplaced granite from the metavolcanics of the Dingyuan Formation in the western Beihuaiyang zone, the Dabie orogen. This study reports the results of zircon U-Pb dating and preliminary petrographic observations on two metagranite samples. The studied rocks experienced epidote-amphibolite facies metamorphism and strong structural deformation. Their U-Pb ages are 726 ± 6 and 758 ± 12 Ma, respectively, similar to those for the Luzhenguan complex in the eastern segment of the Beihuaiyang zone. In combination with previously determined 635 ± 5 Ma low-grade metagabbro, this study suggests the occurrence of at least two types of Neoproterozoic intrusive rocks in the Beihuaiyang zone, the northern margin of the South China Block (SCB): 726–758 Ma metagranite and 635 Ma metagabbro. These rocks occur within the metamorphosed Ordovician volcanic zone (originally named the Dingyuan Formation) and are in tectonic contact to each other, but they formed in different tectonic settings. The protolith ages for the Neoproterozoic low-grade metaigneous rocks are in good agreement not only with ages for two episodes of mid- and late-Neoproterozoic mafic and felsic magmatism in the Suizhou and Zaoyang area, Hubei Province, but also agree with protolith ages of ultrahigh-pressure metaigneous rocks in the Dabie-Sulu orogenic belt. In view of their tectonic relationships to country rocks, it appears that these Neoproterozoic low-grade rocks are exotic and they may have been detached and scraped from subducting SCB crust in the early Triassic during the initial continental subduction, and thrusted over Paleozoic metamorphosed rocks in the southern margin of the North China Block during continental collision. 相似文献
11.
目的探讨准噶尔盆地陆梁地区晚石炭世的构造环境,为限定准噶尔洋的最终闭合时间及进一步研究准噶尔盆地的构造演化提供理论支持。方法根据样品的化学分析数据,运用主量元素、微量元素和稀土元素进行分析。结果研究区火山岩主要为玄武岩,少数为流纹岩、安山岩和英安岩。玄武岩显示板内岩浆演化特征在火山岩构造环境判别图解中处于板内环境,大部分玄武岩Nb/Zr（>0.3）、Th/Nb（0.11～0.20）与陆内裂谷环境相当。结论准噶尔盆地陆梁隆起地区晚石炭世火山岩形成于陆内裂谷环境。 相似文献
12.
为系统解析西非科特迪瓦盆地构造特征、厘定洋陆边界并划分构造单元,明确有利勘探区带,基于新采集地震资料和最新高精度卫星重力数据,应用位场分离技术获取布格重力异常划分科特迪瓦盆地洋陆边界; 利用位场边缘识别技术计算布格重力异常总水平-垂向导数推测控盆断裂6组,其中3组为近东西走向,3组为近南北走向; 利用剩余布格重力异常反演科特迪瓦盆地沉积厚度,根据异常所对应的隆起和坳陷结合布格重力异常和总水平-垂向导数划分东部离散边缘、北部转换离散边缘和洋盆共3个二级构造单元。首次明确了科特迪瓦盆地“东西分段、南北分带”的构造特点、厘定了洋陆边界、划分了构造单元,指出东部离散边缘区为有利勘探区。结合区域地质研究认为东部离散边缘区含油气系统证实,勘探潜力较大,为盆地未来勘探方向。借助高精度卫星重力资料,以区域地质及地震资料为约束,有效解决巨型低勘探盆地构造区划的难题,指明盆地勘探方向,对类似靶区具有较好的借鉴和推广意义。 相似文献
13.
白玲 《鞍山科技大学学报》2011,(5)
利用中国数字地震台网记录的地震波形,观测其穿过地球外核和地幔的SKS波分裂特征,确定了快波S波的振动方向和快慢波时间延迟。这种经过地幔传播的SKS震相的横波分裂主要来源于上地幔的各向异性。可以用应变引起的上地幔中矿物质的结晶优势排列来解释。结果表明,对于所分析的10个观测台站均发现了明显的横波分裂现象。时间延迟在0.4～1.8 s。在东部地区,快波振动方向与中国东北西太平洋俯冲带的板块相对运动方向基本一致,说明俯冲的太平洋板块地幔流对各向异性有重要意义。在西部地区,快波振动方向和时间延迟都具有较大差异,说明其总体形变的起因是复杂的,各向异性受到地幔流和历史构造运动的双重影响。 相似文献
14.
针对刚体飞行动力学难以描述柔性翼飞行器刚柔耦合动力学特性的问题,提出了一种在时域内对刚体运动和弹性体运动交替进行数值计算的建模与循环求解仿真方法.该方法分别为飞行器刚体与弹性体运动建立了独立坐标系,根据坐标系之间的惯性牵连关系,通过气动力与惯性力完成了刚柔耦合动力学关系在刚体与弹性体运动之间的传递.与此对应的仿真算法是在1个积分步长内顺序计算飞行器受力情况、弹性变形状态与刚体运动状态,在仿真步长之间以循环求解的方式进行仿真计算.以飞行器对姿态扰动的动态响应为例进行仿真分析,结果表明本文的动力学建模与仿真方法能正确反映柔性翼飞行器的飞行特性. 相似文献
15.
16.
合肥盆地逆掩冲断带地质-地球物理综合解释及其大地构造属性 总被引：8，自引：0，他引：8
在大量地震剖面综合解释的基础上 ,提出华北板块与北淮阳晚加里东 -早海西期褶皱带的界线应在六安断裂 ,肥中断裂是华北陆壳型基底与其过渡壳型基底的大致分界。首次发现合肥盆地侏罗系之下存在以青白口系刘老碑组泥质岩为主滑脱层的印支期形成的由南向北滑脱冲断、主要卷入华北地台及其被动陆缘上元古 -古生界的完整冲断体系 ,并认为侏罗纪盆地为再生前陆盆地 ,编制了前侏罗系基岩地质图 ,为研究华北、大别及扬子三大块体的相互关系提供了新资料 相似文献
17.
六盘山盆地属于典型的黄土塬地貌沉积盆地,地表条件及地下地质情况复杂,导致二维地震资料信噪比低、静校正难度大、资料品质较差、物探综合解释难度大。综合利用地震合成记录、井正演及野外露头开展地层多元综合标定,明确探区内各组系地层顶底反射界面及其地震反射特征;结合野外构造形迹调查,利用重电震联合约束反演进行相互验证,建立了走滑冲断构造解释模型;通过精细速度分析,建立了研究区速度场,运用模型层析变速成图技术准确落实地下构造。在地质与地球物理技术综合应用基础上,预测有利烃源岩展布区带,部署马参1井。该井钻遇了与预测较为吻合的泥岩及暗色泥岩,并在下白垩统李洼峡组见到了良好的油气显示,证实六盘山盆地西南部确实存在成烃成藏的过程,盆地内马东山构造带是下步勘探的重点区带。 相似文献
18.
三塘湖盆地二叠纪构造层划分及其构造特点 总被引：1，自引：0，他引：1
目的研究二叠纪构造层的划分及其构造特点。方法依据三塘湖盆地二叠纪地层与上覆地层的区域性不整合关系在地震剖面上的反映及其不同构造层的构造变形差异性,划分出二叠纪构造层,并对其构造格局和残留构造特点进行研究。结果二叠纪沉积盖层形成后,遭受晚海西期构造运动的影响,导致中央拗陷带残余二叠纪地层中宽缓褶皱和冲断构造组合的发育;在遭受多期构造叠加改造后,残余的二叠纪构造层在盆地中表现为西南部残余厚度大,东北部残余厚度小的现今构造格局。结论二叠纪构造层具有残留盆地的特征,主要含油层分布在条湖凹陷的西南缘和马郎凹陷。 相似文献
19.
板块汇聚碰撞过程中,常常造成应力矢量与板块边缘的非直交关系,导致平移分量和缩短分量的产生,它们并非不同时期、不同应力场的产物;这种斜向汇聚产生大陆造山带的不对称扇型结构及花状构造,也可能是大陆增生保存的重要形式之一;变形分解作用使得岩石在变形过程中产生纯剪变形分量和单剪变形分量,且不受尺度控制;该理论常被应用于解释造山带尺度的许多构造问题,在秦岭造山带中进行变形分解和板块斜向汇聚研究,有望在理论上有所突破. 相似文献
20.
曹清林 《江苏技术师范学院学报》2005,11(2):18-21,29
研究平面十二杆连杆机构联轴器所有构件和运动副中的力，分析出力与输入力矩以及机构运动位置之间的关系．这些力的最大值将确定相应部分的结构参数大小。最后，通过算例说明具体的计算设计过程。 相似文献