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531.
北大巴山早古生代地幔交代作用与煌斑岩浆的起源和演化 总被引:2,自引:2,他引:0
产于陕西岚皋境内、赋存于碱质煌斑杂岩中的金云角 闪 辉石岩捕虏体是交 代地幔捕虏体。微量元素和SrNd同位素的对比研究表明,金云角闪辉石岩型交代地幔是寄 主煌斑岩的源区。金云角闪辉石岩捕虏体富含高Na、Ti的角闪石是本区寄主煌斑岩富Ti, 具 低K/Na值的根本原因。煌斑杂岩的同位素地球化学研究表明,早古生代地幔交代作用相对 于煌斑岩的侵位是一个相对近的时间间隔,大约发生于距今600~700 Ma。寄主煌斑岩 的 原生岩浆是金云角闪辉石岩型地幔经较大程度部分熔融而形成,原生岩浆为相似于橄榄金伯 利岩和橄辉玢岩的碱质超基性煌斑岩浆,其经初步分离结晶后形成两个不同的母岩浆,分别 相当于橄榄金伯利岩浆和橄辉玢岩岩浆,两个母岩浆各自具有不同的分离结晶系列,形成不 同的岩石类型。 相似文献
532.
533.
从地形变资料探讨丽江7.0级地震的前兆特征 总被引:2,自引:0,他引:2
讨论了地震孕育发生的物理机制是“拉疏隆起-压缩凹陷”模式的形成机理及其特征;根据这一理性认识,应用丽江7.0级地震之前滇西地区的地形变资料,较确切出得出了本区有强震发生,并且可以认为孕震体是在丽江至玉龙雪山东麓地区;根据发震前夕所观测到孕震体的“拉疏隆起-压缩凹陷”的区域大小与幅度值及岩层的弹性应变,可近似计算震级的大小。 相似文献
534.
Parameterized thermal model of a mixed mantle convection 总被引:4,自引:0,他引:4
IntroductionTectonicevolutionisinfluencedbythermalhistoryoftheEarth.TheEarthhasabout4.6Gahistory.ThermalenergyfromtheinterioroftheEachprovidesthemainpowerfortectonicevolution.ItnotonlycontrolstheformationofthelayeredstructuresinsidetheEarth,butalsopromotesthetectonicmovementsofthesurfaceplatesduringthegeologicalera.ThestudyofthethermalhistoryoftheEarthhaspassedseveralstages.Inearlystudies,onlyconductivemechanism(Lubimova,1958)isdiscussedinthethermalevolution.However,theimpotalceofthermalco… 相似文献
535.
536.
Deep xenoliths in alkalic porphyry, Liuhe, Yunnan, and implications to petrogenesis of alkalic porphyry and associated mineralizations 总被引:9,自引:0,他引:9
Xianfan Liu Xinzhi Zhan Zhenmin Gao Jiajun Liu Chaoyang Li Wenchao Su 《中国科学D辑(英文版)》1999,42(6):627-635
Na-rich microlite-glass is first discovered in deep-source xenoliths in alkali-rich porphyry, Liuhe village, Heqing County,
Yunnan Province. It is shown that the ultramafic xenoliths originated from partial melting of primary mantle and the glass
resulted from metasomatism between the xenoliths and mantle fluid derived from mantle degassing. Mantle metasomatism not only
resulted in the enrichment of alkaline, large-ion elements, ore metals and volatiles but also created a favorable condition
for the generation of alkaline magmas. The mantle xenoliths and their characteristics of mantle metasomatism provide important
evidence for a better understanding of the petrogenesis and mineralization of the Cenozoic alkali-rich porphyry in western
Yunnan. 相似文献
537.
大同—阳高震区深部构造背景 总被引:6,自引:0,他引:6
利用通过本区的宽角反射/折射剖面资料对大同-阳高震区及邻区地壳上地幔速度结构与构造进行了详细的研究,结果表明,地壳上地幔速度结构与构造在纵向和横向上具有明显的不均一性,浅部基底断裂发育,对应其深部,根据波组特征,壳内界面及速度等值线起伏变化和低速异常体的边界等推测了地壳深断裂带,区内最明显的上地壳低速体位于大同-阳原附近,其南界存在地壳断裂,大同-阳高地震群与该低速异常体和深断裂有关。 相似文献
538.
Orozco Miguel Molina José Miguel Crespo-Blanc Ana Alonso-Chaves Francisco Manuel 《Geologie en Mijnbouw》1999,78(1):103-117
The rauhwackes near Serón in the northern Sierra de los Filabres (S Spain), previously considered as true tectonic breccias, are reinterpreted on the basis of sedimentological, geomorphological and geometrical evidence as subaerial or nearly subaerial sedimentary deposits. Channel fills, parallel lamination, cross-lamination, graded bedding, sedimentary clastic dykes and other sedimentary structures and features occur in the rauhwacke body. These sedimentary rocks correspond to continental deposits of alluvial and karstic origin deposited over a karstified erosional surface of Nevado–Filabride marbles. Although no fossils have been found in the rauhwackes, a Tortonian age for these rocks is suggested on the basis of structural arguments and lithostratigraphic data from the nearby Almanzora basin. The rauhwackes were buried by slabs of Alpujarride rocks that gravitationally slid over them during the uplifting of the Sierra de los Filabres. 相似文献
539.
The age of continental roots 总被引:39,自引:0,他引:39
D. G. Pearson 《Lithos》1999,48(1-4):171-194
Determination of the age of the mantle part of continental roots is essential to our understanding of the evolution and stability of continents. Dating the rocks that comprise the mantle root beneath the continents has proven difficult because of their high equilibration temperatures and open-system geochemical behaviour. Much progress has been made in the last 20 years that allows us to see how continental roots have evolved in different areas. The first indication of the antiquity of continental roots beneath cratons came from the enriched Nd and Sr isotopic signatures shown by both peridotite xenoliths and inclusions in diamonds, requiring isolation of cratonic roots from the convecting mantle for billions of years. The enriched Nd and Sr isotopic signatures result from mantle metasomatic events post-dating the depletion events that led to the formation and isolation of the peridotite from convecting mantle. These signatures document a history of melt– and fluid–rock interaction within the lithospheric mantle. In some suites of cratonic rocks, such as eclogites, Nd and Pb isotopes have been able to trace probable formation ages. The Re–Os isotope system is well suited to dating lithospheric peridotites because of the compatible nature of Os and its relative immunity to post-crystallisation disturbance compared with highly incompatible element isotope systems. Os isotopic compositions of lithospheric peridotites are overwhelmingly unradiogenic and indicate long-term evolution in low Re/Os environments, probably as melt residues. Peridotite xenoliths from kimberlites can show some disturbed Re/Os systematics but analyses of representative suites show that beneath cratons the oldest Re depletion model ages are Archean and broadly similar to major crust-forming events. Some locations, such as Premier in southern Africa, and Lashaine in Tanzania, indicate more recent addition of lithospheric material to the craton, in the Proterozoic, or later. Of the cratons studies so far (Kaapvaal, Siberia, Wyoming and Tanzania), all indicate Archean formation of their lithospheric mantle roots. Few localities studied show any clear variation of age with depth of derivation, indicating that >150 km of lithosphere may have formed relatively rapidly. In circum-cratonic areas where the crustal basement is Proterozoic in age kimberlite-derived xenoliths give Proterozoic model ages, matching the age of the overlying crust. This behaviour shows how the crust and mantle parts of continental lithospheric roots have remained coupled since formation in these areas, for billions of years, despite continental drift. Orogenic massifs show more systematic behaviour of Re–Os isotopes, where correlations between Os isotopic composition and S or Re content yield initial Os isotopic ratios that define Re depletion model ages for the massifs. Ongoing Sr–Nd–Pb–Hf–Os isotopic studies of massif peridotites and new kimberlite- and basalt-borne xenolith suites from new areas, will soon enable a global understanding of the age of continental roots and their subsequent evolution. 相似文献
540.
K. Priestley 《Lithos》1999,48(1-4):45-56
The velocity model for southern Africa of Qiu et al. [Qiu, X., Priestley, K., McKenzie, D., 1996. Average lithospheric structure of southern Africa. Geophys. J. Int. 127, 563–587] is revised so as to satisfy both the regional seismic waveform data and the fundamental mode Rayleigh wave phase velocity data for the region. The revised S-wave model is similar to the original model of Qiu et al. except that the high velocity, upper mantle lid extends to 160 km depth in the revised model rather than to 120 km in the original model. Sensitivity tests of the regional seismic data show that the minimum velocity in the S-wave low velocity zone can be as high as 4.45 km s−1 compared to 4.32 km s−1 in the Qiu et al. model. The vertical S-wave travel time for the revised south African model is compared with the vertical S-wave travel times for the global tomographic models S12WM13 and S16B30, and they are found to be similar. 相似文献