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1.
使用２０多万个ＭＡＧＳＡＴ卫星磁测数据，编绘亚洲卫星标量（△Ｆ）和矢量（△Ｘ，△ｙ，△Ｚ）磁异常图（２０°ｓ－６０°Ｎ，５０°Ｅ－１６０°Ｅ）．为了提取岩石层卫星磁异常，首先对ＭＡＧＳＡＴ卫星数据进行了筛选，然后进行主磁场、磁层场、电离层场和感应场改正，并消除虚假测点．将卫星数据分成黎明组、黄昏组和联合组，分别绘制相应的卫星磁异常图．根据１°×１°的网点值，用计算机编绘亚洲卫星磁异常图．初步分析了卫星磁异常与大地构造的关系． 相似文献
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GRACE重力卫星任务即将结束,后续GRACE Follow-On卫星计划于2017年发射,在此期间,迫切需要一个新的卫星计划继续对全球时变重力场进行连续监测,以保证时变重力场信息时间序列的连贯性.SWARM计划包括三颗轨道高为300~500 km的近极轨卫星星座,类似于三颗CHAMP卫星,具有接替时变重力场探测的潜力.本文首先分析SWARM(模拟)、CHAMP、GRACE反演至60阶时变重力场球谐系数的误差特性及不同高斯平滑半径对高频误差的抑制效果,然后分别利用SWARM、CHAMP、GRACE的时变重力场模型恢复全球质量变化,结果表明,SWARM模拟观测数据的高频误差低于CHAMP观测数据,探测时变重力场的整体精度优于CHAMP,略低于GRACE探测精度;其次,对比2003年1月—2009年12月期间CHAMP(hl-SST)和GRACE(ll-SST)时变重力场模型反演格陵兰岛冰盖质量变化趋势,结果显示,CHAMP数据得到格陵兰岛冰盖质量变化趋势为-50.2±2.0 Gt/a,GRACE所得结果为-41.2±1.6 Gt/a,两者相差21.8%;最后,对比2000年1月—2004年12月间SWARM模拟数据和"真实"模型数据反演的格陵兰岛冰盖质量变化趋势,结果表明,两者相差19.2%.本文研究表明,利用SWARM hl-SST数据探测时变重力场可以达到20%相对精度水平,有潜力用于填补GRACE和GRACE Follow-On期间探测地球时变重力场的空白. 相似文献
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本文利用CHAMP卫星磁测资料建立的新一代高阶地磁场模型POMME-4.2S,计算中国及邻区400 km高度的卫星磁异常及其垂直梯度,给出7个磁场分量的分布图,比较了截断水平对磁异常分布的影响,初步分析了磁异常与岩石圈构造的关系.主要结果表明,在四川盆地、塔里木盆地和松辽盆地等主要磁异常区,ΔZ异常中心的南北两边出现ΔX的异常中心,东西两边出现ΔY的异常中心.在球谐模型为90阶时,磁异常分布的基本形态已经确定,更高的模型阶数对磁异常只有微小调整.在磁异常较强的地区,磁异常及其垂直梯度同步变化.卫星磁异常与地形变化、断裂带分布、莫霍面深度和岩石圈厚度没有直接的对应关系,而与居里等温面深度、磁性层厚度有明显的相关性.居里等温面深、磁性层较厚的地区显示正磁异常,居里等温面浅、磁性层较薄的地区显示负磁异常. 相似文献
4.
用矩谐分析的方法研究了中国及其邻域（φ=10°-60°N,λ=70°-140°E）由MAGSAT卫星获得的地磁矢量异常数据,求出了卫星高度400km处的矩谐模型.据此模型,绘出了高度400km处矩谐模型的理论磁异常图.结果表明,ΔX,ΔY,ΔZ图上有很强的区域磁异常特征,新疆地区天山、阿尔泰山、塔里木地区为很强的正异常,青藏高原和喜马拉雅山一带则为负异常区,说明这些地区存在着很强的局部磁化. 相似文献
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利用GRACE卫星重力场模型和地表流动重力观测资料,计算2008年汶川MS 8.0地震发生前6年的重力变化,对卫星和流动重力段差结果与卫星重力反映的重力场动态变化特征进行研究,结果表明：①GRACE卫星重力段差受滤波半径影响显著,与地表流动重力观测结果相比,在重力变化数值上差异较大,在变化率上较为一致;②在汶川地震孕育阶段,川滇地区重力等值线呈“增大—减速增大—减小”的特征,震前2年形成近似垂直于龙门山断裂带的重力变化梯度带。 相似文献
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利用最新的波茨坦地磁场球谐模型(Potsdam Magnetic Model of the Earth,POMME)进行仿真实验,分别模拟出不同卫星轨道高度下的磁测数据.根据仿真的观测数据反演地壳磁场的高斯球谐系数,对反演结果进行对比和分析,总结出卫星轨道高度对反演结果的影响.针对CHAMP卫星实测数据进行地壳磁场反演,由不同轨道高度磁测数据反演得到的磁场(Magnetic Field,MF)系列模型,验证卫星轨道高度对反演的影响,从而为磁测卫星系统设计论证指标中的卫星轨道高度设计提供一定的参考和指导. 相似文献
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为了整体了解青藏高原东南缘龙门山断裂带的卫星重力场特征及其发震机制,文中基于重力卫星数据展现出研究区域的地形信息,并通过解算反映莫霍面起伏的区域重力异常,反演出研究区域的莫霍面深度,同时运用GPS速度场数据探测了研究区域地壳的形变速率及方向;最后,结合龙门山断裂带的构造背景及前人已有的深部探测结果,分析其发震前后重力时变场的动态特征并探讨了发震机理。研究结果表明:青藏高原东缘深部物质逐年向E流展,在龙门山断裂带处强势受阻,持续的挤压、碰撞过程形成了深部莫霍面的"陡降带",长期的应力作用利于逆冲推覆和走滑构造的形成;龙门山地震带震前处于明显的重力变化梯度带,深部物质运移的流速差异大,流体压力增强,有助于地壳流体入侵和软流圈物质底侵上涌;物质和能量的持续积累最终将导致深部应力严重失衡、深部薄弱构造剪切破裂,从而发生逆冲、推覆构造运动的大地震。 相似文献
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《地球物理学进展》2020,(3)
本文以焦家断裂带为研究目标,综合利用地质、重力、磁法、大地电磁等资料,总结了区域物性、重磁场特征,并选择典型剖面,利用实测MT数据,开展了2.5D重磁电联合精细反演,推断了控矿断裂构造的深部变化特征.A-A′剖面重磁电特征显示,焦家断裂带上盘呈现低阻-中磁特征,而下盘呈现高阻-高磁特征,焦家断裂带和三山岛断裂带的视电阻率异常梯度带在4 km以浅非常清晰,分界线走势基本沿焦家断裂带深部延伸,呈现"漏斗"形状.本文根据建立的地质-地球物理找矿预测模型推断,焦家断裂带剖面上低磁异常向高磁异常的过渡带、布格重力异常梯级带的转弯部位和视电阻率等值线同步向下弯曲、间距变大及由陡变缓部位都是成矿的有利部位,为今后该地区金矿勘查提供重要技术指导. 相似文献
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根据亚洲地区（15°S-60°N,55°E-160°E）MAGSAT卫星碰异常1°×1°网格值,使用冠谐分析方法,计算亚洲地区卫星磁异常的冠谐模型．球冠极点位于22°N,108°E;球冠半角为50°．该模型的最大截断指数Kmax=20,共有441个系数．根据冠谐模型,绘制卫星平均高度（400km）以及其他高度（300km和500km）的理论卫星磁异常图（△X,△Y,△Z）．卫星磁异常的冠谐模型能表示磁异常的三维结构,为探讨岩石层结构提供证据． 相似文献
11.
Sub-ice geology inland of the Transantarctic Mountains in light of new aerogeophysical data 总被引：3，自引：0，他引：3
Michael Studinger Robin E. Bell W.Roger Buck Garry D. Karner Donald D. Blankenship 《Earth and Planetary Science Letters》2004,220(3-4):391-408
The Transantarctic Mountains are a major geologic boundary that bisects the Antarctic continent, separating the low-lying, tectonically active terrains of West Antarctica from the East Antarctic craton. A new comprehensive aerogeophysical data set, extending 1150 km from the Ross Sea into the interior of East Antarctica provides insights into the complex structure inland of the Transantarctic Mountains. Geophysical maps, compiled from 21 000 km of gravity, magnetic and subglacial topography data, outline the boundaries of several geologic and tectonic segments within the survey area. The coherent pattern in magnetic data and mesa topography suggests a subglacial extent of the Transantarctic Mountains 400–500 km inland the last exposed rock outcrops. We estimate the maximum thickness of a potential sediment infill in the Wilkes Subglacial Basin to be less than 1 km, based on gravity modeling and source depth estimates from magnetic data. The coherent nature of the potential field and topography data, together with the northwest–southeast trends, define the Adventure Subglacial Trench and the Resolution Subglacial Highlands as a tectonic unit. The crustal structure and the strong similarity of the observed gravity with fold-and-thrust belts suggest a compressional scenario for the origin of the Adventure Subglacial Trench and the Resolution Subglacial Highlands. The complexity and apparent structural control of the Wilkes Subglacial Basin raise the issue of what influence pre-existing structures may have played in the formation of the Transantarctic Mountains system. The previous hypothesis of a thermal boundary beneath the mountains is difficult to reconcile with our new gravity data. The apparent difficulties to match our new data with certain key aspects of previous models suggests that a reassessment of the existing uplift models is necessary. We have modeled the prominent gravity anomaly over the Transantarctic Mountains with thicker crust. 相似文献
12.
东海陆架盆地及其周边海域地质、地球物理场特征 总被引：7，自引：5，他引：7
分东海陆架盆地及其周边海域的重、磁场特征、对研究区域的地球物理场资料进行了小波变换与多尺度分布与计算，计算了研究了海域重，磁资料的1－4阶小波变换逼近、细节、根据分析与计算可知，在东海陆架盆地及其周边域，重、磁异常的主要特征没有内陆盆地那样明显，但盆地内的绝大部分地区均位于异常相对缓变区，在盆地内部有时有局部异常的圈闭及剧变区，但总的特征为缓变的，而周边区域多为相对剧变区，但也存在局部区域的缓变, 、磁场特征表明，盆地基底相对盆地周边区域主要由密度较大，磁性中的岩石组成，因此盆地中部以高正磁异常为主，布格重力异常 对周边地区高，东海陆架盆地及其周边海域的重力场的主要走向为NNE向，局部重力异常较为平缓，磁异常走向没有重力异常明显，但主要也为NNE向，重、磁场的分布特征表明，东海陆架盆地及其邻域的地质构造为大陆架构造的延伸。 相似文献
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GRACE卫星的成功发射为海底沉积物的监测提供了新的方法.利用2003-2014年间的GRACE RL05数据，采用同期的测高数据对海面高变化进行改正，使用水文模式数据和基于均一假设的尺度因子估计方法处理泄漏误差，反演了东海地区的沉积物变化情况，并对GIA效应进行了改正.结果表明：东海入海口处沉积物的平均变化速率为5.44±0.88 mm·a-1，最大值出现在浙江沿海地区，变化速率为6~7 mm·a-1；在空间分布上，呈现河口处沉积速率大，远离河口的大洋地区沉积速率小的特征.在时空分布上均与实测数据很好的吻合.沉积物变化时间序列的周年项振为6.8 cm，周年变化主要与东海泥沙扩散路径相关的海洋环流模式有关；半周年项和两周年项振幅分别为0.6 cm和0.7 cm，这两项变化主要与长江流域降水引起的土壤侵蚀变化有关.最后，分析讨论了本文沉积物监测方法推广到其他地区的适用性和局限性. 相似文献
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D.C. Mishra 《Earth and Planetary Science Letters》1977,36(2):301-308
Geophysical data contiguous with the Narmada-Son lineament suggests its possible extension westward into the Arabian Sea and eastward up to the Shillong Plateau. The airborne magnetic anomaly map of the north Arabian Sea delineates a linear trend of magnetic anomalies in line with the Narmada-Son lineament. This group of magnetic anomalies, spreading over 20°N to 22°N, starts near the west coast of India at 21°N, 69°30′E and extends to the Murray Ridge. The tectonic feature represented by this group of magnetic anomalies is buried by a thick layer of sediments. This westward extension of the lineament is also reflected in the average Bouguer gravity anomaly map of the Indian Ocean. Towards the east, the gravity and magnetic data delineate a subsurface linear tectonic feature which extends in line with this lineament to the eastern syntaxial bend. These various geophysical signatures further suggest the lineament to be a typical rift-like structure. The tectonic implications of the lineament, which extends from the western to the eastern margins of the Indian plate, is discussed. 相似文献
15.
A Bouguer gravity anomaly map is presented of the North Sea and adjacent land areas in Norway and Denmark, covering an area situated between 56° and 62°N, 1°W and 10°E. The gravity data from the UK sector of the North Sea, the land and offshore areas of Denmark, and the land areas of Norway have been published before. However, the gravity data from the Norwegian sector of the North Sea are new. A large number (about 60) of individual gravity features can be defined in the mapped area. Most of those situated in the UK sector of the North Sea and on land in Norway have been discussed earlier; however, most of the anomalies found elsewhere which are qualitatively interpreted here have not been discussed before. An interpreted Bouguer anomaly map is presented which identifies all these features. The majority of the gravity anomalies encountered in the mapped area can be shown to be associated with one of the following geological features: (i) basement highs, (ii) large bodies of heavy basic or ultrabasic rock in the crystalline basement, (iii) large igneous intrusions within the sedimentary column and thick accumulations of volcanic rocks or their associated eruption centers, (iv) major basement faults. Large-scale geological structures such as the Central, Viking and Sogn Grabens and the East Shetland, Stord, Forth Approaches and Norwegian-Danish Basins are essentially in isostatic equilibrium and are only locally marked by relatively weak gravity minima. A residual gravity anomaly map has been produced by subtracting from the observed Bouguer anomalies the estimated gravity effect of an assumed thinned crust. This residual gravity anomaly map shows a number of features of the Bouguer anomaly field with greater clarity. 相似文献
16.
综合地震层析成像与重磁数据的处理结果，选择26°N～36°N，120°E～130°E的范围作为研究区，讨论了黄、东海研究区的深部结构特点及其与周边各地质单元的相互关系，完成了研究区两条剖面的密度结构反演，认为东海陆架地区地壳厚度变化与大陆地区相比并不明显，显著减薄开始于冲绳海槽地区，中地壳消失；琉球岛弧处地壳厚度明显再度增加，特别是上地壳的厚度增加最大，推断其原因应与俯冲作用及俯冲带附近板块与地幔的运动速率之差有关.地球物理场“东西分带”是黄海—东海地区壳内结构从西向东变化的反映，但随着深度的增加，研究区的岩石层结构出现以近EW向为优势的构造格局.因此推断深部近EW向的异常是三叠纪时期南北板块碰撞、挤压所致，浅部的NE向条带异常是后期构造运动在岩石层较浅部位构造效应的反映.黄海—东海地区岩石层结构存在浅部与深部优势构造方向不协调的现象.层析成像结果证实了南黄海东缘断层的存在，还勾绘出绍兴—十万大山碰撞带为以40°左右的倾角向NW方向倾斜的高速带，另一条倾向基本相同的高速带则是南、北扬子块体结合带在深部的反映. 相似文献
17.
Luning Shang Xunhua Zhang Runlin Du Yonggang Jia Zhenxing Tian Bo Han Chuansheng Yang 《Studia Geophysica et Geodaetica》2016,60(4):679-699
In September and October of 2011, a marine magnetic survey was conducted in the southern East China Sea between 120° and 126°E, 26° and 28°N with the research vessel Kexue-3. New magnetic maps with 5 × 5 km grid spacing were generated after meticulous data processing. Based on an analysis of magnetic anomaly features and further calculation results, including the total horizontal derivatives (THD), second order vertical derivatives (SVD) and analytic signal amplitude (ASA), several new tectonic insights on magnetic sources, basement structures and fault properties were obtained. The NE-SW or NNE-SSW oriented magnetic anomaly highs have different sources: (1) The high amplitude, short wavelength magnetic anomalies of the Zhemin Uplift are caused by shallow buried igneous rocks intruded along NE-NEE oriented faults. (2) The high amplitude, moderate wavelength magnetic anomalies of the Diaoyudao Uplift are caused by the metamorphic basement intruded by magmatic rocks. (3) The magnetic sources of the Yandang Uplift and Taibei Uplift in the shelf basin are shallow buried metamorphic basements and deep buried volcanic bodies, respectively. Several NW-SE or NWW-SEE oriented dextral strike-slip fault belts were identified as important tectonic boundaries. Each is composed of several en echelon and partly overlapping secondary faults. Initially formed in the Cretaceous, these fault belts have evolved through multiple periods, propagated seaward with the migration of the basement rifting and accommodated local stress fields in the Cenozoic. 相似文献
18.
南海深部构造对研究南海构造演化和油气勘探具有重要意义.本文对南海地区的自由空气重力异常进行布格校正、海水层校正和沉积层校正，得到布格重力异常，再对布格重力异常进行区域异常和局部异常分离，利用位场界面反演方法对区域布格异常进行反演计算得到研究区域的莫霍面深度分布；采用全变倾角化极方法对研究区域的卫星磁异常数据进行化极处理，并进一步对化极磁异常作向上延拓，得到延拓后化极磁异常结果.分析布格重力异常、莫霍面深度及化极磁异常特征，结合天然地震层析成像的证据，得到以下结论：推测南海北部陆缘的古俯冲带位置是从118.5°E，24°N沿北东向延伸至109°E，15°N；红河断裂入海后经过莺歌海盆地在海南岛南部转为南北向与越东断裂相接并延伸至万安盆地；推测中特提斯洋的部分闭合位置是从110°E，2°N到101°E，21°N. 相似文献