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1.
通过1:5万地质填图工作,将叶柏寿隆起区的早前寒武纪建平群变质岩进行了解体。新的研究成果表明区内基底岩系主要由晚太古代TTG和CA质侵入杂岩及少量表壳岩,早元古代变质火山-沉积岩组成。阳老的表壳岩呈捕掳体状分布在TTG,CA质侵入杂岩中,CA持杂岩侵入TTG质杂岩中。  相似文献   

2.
北京地区太古宙岩石同位素年龄及其意义   总被引:7,自引:0,他引:7  
北京地区太古宙大漕-沙厂表壳岩系的麻粒岩相区域变质作用年龄,苇子峪TTG(A)-M-Me杂岩中表壳岩系的高角闪岩相区域变质作用年龄,以及两个单元中的早期TTG质岩成岩年龄均为2650Ma左右,推测表岩成岩时人代为中太古代晚期,四合堂表壳岩系的低角闪岩相区域变质作用年龄和该单元内太古宙TTG质岩的成岩时代约为2539Ma至2580.7Ma推测表壳岩系成岩时国新太古代早期(2650~2800Ma)阳坡  相似文献   

3.
通过1∶5万地质填图工作,将叶柏寿隆起区的早前寒武纪建平群变质岩系进行了解体。新的研究成果表明区内基底岩系主要由晚太古代TTG和CA质侵入杂岩及少量表壳岩,早元古代变质火山—沉积岩组成。最老的表壳岩呈捕掳体状分布在TTG、CA质侵入杂岩中,CA质杂岩(辘轳井二长片麻岩)侵入TTG质杂岩(叶柏寿片麻杂岩)中。  相似文献   

4.
库鲁克塔格地区新太古代深沟片麻杂岩特征   总被引:10,自引:2,他引:8  
新疆库鲁克塔格地区深沟片麻杂岩是由新太古代阜平期表壳岩组合、灰色片麻岩及古元古代红色片麻岩组成的杂岩体。表壳岩组合为变火山-沉积岩、灰色片麻岩为太古宙TTG岩浆岩组合,红色片麻岩为深沟变质核杂岩同构造侵入的“I”型花岗岩。深沟片麻杂岩组成内核,古元古界兴地塔格岩群组成滑脱系,古元古界南辛格尔塔格岩组组成盖层,它们构成一个完整的深沟变质核杂岩构造。灰色片麻岩、表壳岩组合的Sm-Nd全岩等时线年龄(2830.2±79.7)Ma,红色片麻岩锆石U-Pb年龄(2059±14)Ma。  相似文献   

5.
崤山地区太古代变质花岗岩地质地球化学特征   总被引:1,自引:0,他引:1  
庞振山  梁天佑 《河南地质》1997,15(4):278-282
崤山地区原“太华群”由15%的变质表壳岩和85%的变质花岗岩组成。变质花岗岩的主要岩石类型有;石英闪长岩,英云闪长岩,奥长花岗岩,花岗闪长岩。通过对变质花岗岩的地质,地球化学研究表明,崤山地区太古代变质花岗岩与国内外其他地区的TTG岩系类似。根据野外接触关系和一组锆石Pb-Pb蒸发年龄,确定其成岩时代为太古代。  相似文献   

6.
胶东群新议   总被引:2,自引:0,他引:2  
太古代胶东群主要是由TTG花岗质片麻岩组成。近期区调研究发现真正的变质表壳岩系仅在其中呈包体出现,据岩性特征胶东岩群可分为苗家岩组、郭格庄岩组,时代为晚太古代  相似文献   

7.
山东沂水紫苏花岗岩特征-形成时代及成因探讨   总被引:8,自引:0,他引:8       下载免费PDF全文
苏尚国   《地球科学》1999,24(1):57-62
通过对山东沂水地区紫苏花岗岩野外地质特征、岩相学及地球化学特征等的研究,认为山东沂水地区紫苏花岗岩为变质表壳岩经深熔作用形成.其主要证据为:(1)紫苏花岗岩与变质表壳岩在空间上密切伴生,二者多为渐变过渡接触关系,且他们的片麻理协调一致;(2)在变质表壳岩中发育大量长英质或花岗质脉体,这些脉体的矿物成分、地球化学特征与紫苏花岗岩一致;(3)紫苏花岗岩与变质表壳岩具有相似的稀土配分型式;(4)紫苏花岗岩亏损大离子亲石元素及生热元素,其原岩应为经历了深变质作用的岩石;(5)紫苏花岗岩中锆石多为圆粒状和椭球状,并发育磨蚀坑,说明其原岩主要为变沉积岩;(6)麻粒岩相变质作用时间与紫苏花岗岩形成时间基本一致.  相似文献   

8.
白瑾  戴凤岩 《地学前缘》1997,4(4):281-289
在中条山,古太古代-中太古代的涑水杂岩主要由TTG岩套组成,另有一些表壳岩残体和基性岩墙群。以不整合覆于其上的新太古代绛县群由不成熟的浊积岩和双峰式火山岩组成,沉积于类似现代活动大陆边缘的构造环境,遭受了低绿片岩相至低角闪岩相的变质和强烈的变化。  相似文献   

9.
崤山太古宙花岗—绿岩地体的地质特征   总被引:1,自引:0,他引:1  
崤山太古宙花岗-绿岩地体由15%的绿岩带(变质表壳岩系)和85%的花岗质片麻岩系(变质侵入岩)组成。呈包体产出的绿岩系分为以变火山岩为主的兰树沟岩组和以变沉积岩为主的杨寺沟岩组。花岗质片麻岩包括早期富钠的TTG质花岗岩和稍后的富钾花岗岩。晚期则有代表大陆地壳裂解的基性岩墙群侵入。文中介绍了各岩石单元的地质、地球化学特征及花岗-绿岩带的变形和变质特征,探讨了研究区太古宙的大陆地壳演化。  相似文献   

10.
为了确定鲁西莲花山地区新太古代晚期二长花岗岩中的表壳岩包体的形成时代,并探讨与相邻雁翎关地区的雁翎关岩组中的新太古代早期变质火山岩系的关系。本文对表壳岩包体及相关岩石进行了锆石年代学和地球化学研究。表壳岩包体主要由变质超基性岩和斜长角闪岩组成,另含少量(黑云)角闪变粒岩和黑云变粒岩。SHRIMP锆石U-Pb定年结果显示:角闪变粒岩的岩浆锆石年龄为2 757 Ma;侵入斜长角闪岩的奥长花岗岩脉的年龄为2 593 Ma;从变质超基性岩分选出很少锆石,它们普遍遭受强烈变质重结晶,207Pb/206Pb年龄为2 657~2 397 Ma。变质超基性岩具轻稀土亏损型或平坦型稀土模式,斜长角闪岩具平坦型稀土模式,角闪变粒岩具轻稀土略富集稀土模式,虽然大离子亲石元素相对富集,但都无明显Nb、Ta亏损。表壳岩包体的岩石组合、地球化学组成特征和形成时代可与相邻雁翎关地区的雁翎关岩组中的新太古代早期变质火山岩系对比,形成于大洋环境。新太古代早期表壳岩的原有分布范围应比现在所见到的更为广泛。  相似文献   

11.
东濮凹陷北部沙三中亚段广泛发育盐岩和烃源岩,这两个看似不能共存的物质却在这里互层共生。该时期研究区沉积特征为多盐韵律与多层烃源岩互层共生、连续沉积,单个盐韵律厚度从几米到十几米,烃源岩有机质丰度高、类型好。平面上,两者在湖盆沉积沉降中心共生;垂向上,高有机质丰度、好干酪根类型与高盐度地层具有较好的对应关系。因而成为恢复古气候和古环境的重要研究对象。通过岩石学、古生物学以及Sr/Ba、B/Ga、(V+Ni+Mn)、Fe/Mn、Sr/Cu、Mg/Ca、V/(V+Ni)、稀土元素含量和氯同位素等方法对凹陷北部沙三中亚段的沉积环境进行研究。结果表明,凹陷北部沙三中亚段为深水沉积的还原环境,古盐度较高,达到半咸水-咸水沉积;微量元素和孢粉化石特征表明研究区沙三中亚段为温暖潮湿的环境。  相似文献   

12.
In order to characterise the influence of the heavyrains on the observed landslides during the 1996–1997hydrological cycle, rainfall records for the last 100years are analysed from 104 stations in easternAndalusia. Regarding the amounts of rain recordedbetween October 1996 and March 1997 in the 104stations studied, 31 presented new all-time records;15 presented values that were 80–100% of thepre-1995 record; 49 stations, 80–50%; and 9stations, < 50%. A map has been devised of thesusceptibility of the materials through which thesouth-eastern Andalusian road network crosses,together with an inventory of the damage caused byinstability phenomena on banks and cuttings of theroad network during the winter of 1996–1997. Therelationships between the rainfall during the studyperiod, the damage caused to the road network and thesusceptibility of the materials affected are analysed.The results indicate that there is a clearcorrespondence between the rainfall recorded and thesusceptibility of the materials with the inventorieddamage. It is concluded that the widespread seriousdamage caused in early 1997 to the roads andsurrounding areas in the Alpujarra region and thecoast of the Province of Granada was mainly caused bythe extraordinarily heavy rains. However, considerablyless damage was observed where the susceptibility ofthe terrain is low, thus highlighting the extremeusefulness of terrain-susceptibility maps for riskprevention and territorial planning.  相似文献   

13.
郯庐断裂南段研究进展与断裂性质讨论   总被引:13,自引:3,他引:13  
据1:5万区域地质调查和专题研究资料,就郯庐断裂带是否南延与消失的原因,其与大别—苏鲁造山带交截形成的假位错效应,以及与中新生代沉积盆地形成演化的关系等作了新的阐述。在此基础上,讨论了郯庐断裂带是否为巨大的左行平移断层或转换断层。认为郯庐断裂带可能是在“古郯庐带”的基础上于早侏罗世重新活动、白垩纪强烈活动的地堑型枢纽断裂带。  相似文献   

14.
塘口水电站大坝基础座落在断层和裂隙较发育的龟裂纹灰岩上,岩体完整性差、透水性强,多年运行后,大坝灌浆廊道和排水廊道出现多处集中性漏水,为确保大坝安全和电站正常发电,根据渗漏性质和成因,采用对灌浆廊道补充帷幕灌浆,对排水廊道进行固结+帷幕+回填灌浆。通过灌浆处理后,效果良好,表明灌浆工程有效的将导致坝基渗漏的上下游的裂隙通道封闭,并顺利的经受了随后的汛期洪水考验,大坝安全得到保障。  相似文献   

15.
International unity is becoming ever stronger in this country owing to an increasing similarity in the development of the cultural environment. This comprises the provision of all the country's republics with a sufficient number of schools, theatres, and other institutions and cultural information media in accordance with the needs of the population. An important part is played by the rise in ‘the general educational level, as well as the level of professional qualifications and skills. Among all the Soviet nations and nationalities, this rise being more rapid among formerly backward peoples. Prominent among the factors of internationalization is the progressive development of the nationalities’ cultural resources, while professional culture is being increasingly brought within the reach of the masses.The implementation of the nationalities policy promotes the all-round development of all Soviet nations and nationalities, their drawing together, the upsurge of the individual capabilities of every Soviet citizen.  相似文献   

16.
某高速公路下伏煤矿采空区稳定性分析   总被引:10,自引:0,他引:10  
在论述某高速公路下伏砦脖煤矿采空区地质、采矿和工程地质特征的基础上, 进行了稳定性数值模拟分析, 定性与定量地分析与评价了该煤矿采空区的地表变形特征及稳定性。研究结果表明: 该煤矿采空区的变形尚未完成, 对拟建的高速公路将产生很大的危害, 必须采取相应的工程治理措施。   相似文献   

17.
The Global Stratotype Section and Point (GSSP) for the base of the Silurian System was defined in 1985. Since that time, a number of researchers have suggested that this section has serious deficiencies for use as a GSSP. As a result, in 2000, the Subcommission on Silurian Stratigraphy (SSS) proposed undertaking a formal restu@ of this GSSP, which was subsequently approved by the International Commission of Stratigraphy (ICS). The result of this restudy was the formal proposal that the current GSSP, at 1.6 m above the base of the Birkhill Shale, at Dob's Linn, Scotland, should be maintained as the same locality and stratigraphic level, but the bios- tratigraphical definition of the boundary should be revised. The previously defined, basal Silurian grapto- lite zone, the Parakidograptus acuminatus Zone, should be subdivided into a lower Akidograptus ascensus Zone and a higher E acuminatus Zone. The base of the A. ascensus Zone, marked by the first appearance of A. ascensus, should be regarded as the biostratigraphic mark for the base of the Silurian. This proposal has now been formally approved by the SSS and ICS, and ratified by International Union of Geological Sciences. This is the first GSSP to undergo formal restudy and redefini- tion, and the proposal also included a recommended procedure for restudy of GSSPs.  相似文献   

18.
In reservoir characterization, the covariance is often used to describe the spatial correlation and variation in rock properties or the uncertainty in rock properties. The inverse of the covariance, on the other hand, is seldom discussed in geostatistics. In this paper, I show that the inverse is required for simulation and estimation of Gaussian random fields, and that it can be identified with the differential operator in regularized inverse theory. Unfortunately, because the covariance matrix for parameters in reservoir models can be extremely large, calculation of the inverse can be a problem. In this paper, I discuss four methods of calculating the inverse of the covariance, two of which are analytical, and two of which are purely numerical. By taking advantage of the assumed stationarity of the covariance, none of the methods require inversion of the full covariance matrix.  相似文献   

19.
It is known from observations that the center of mass of the Moon does not coincide with the geometric center of its figure, and the line connecting these two centers is not aligned with the direction toward the center of the Earth, instead deviating toward the Southeast. This stationary deviation of the axis of the inertia ellipsoid of the Moon to the South of the direction toward the Earth is analyzed. A system of five linear differential equations describing the physical libration of the Moon in latitude is considered, and these equations are derived using a new vector method taking into account perturbations from the Earth and partly from the Sun. The characteristic equation of this system is obtained, and all five oscillation frequencies are found. Special attention is paid to the fifth (zero) frequency, for which the solution of the latitude libration equations are stationary and represents a previously unknown additional motion of the rotational axis of theMoon in a cone with a small opening angle. In contrast to the astronomical precession of the Earth, the rotation of the angular-velocity vector is in the positive direction (counter-clockwise), with the period T 3 = 27.32 days. On this basis, this phenomenon has been named “quasi-precession.” This quasi-precession leads to a stationary inclination of the major axis of the inertia ellipsoid of theMoon to the South (for an observer on Earth), making it possible to explain one component of the observed deviation of the center of mass of the Moon from the direction toward the Earth. The opening angle of the quasiprecession cone is approximately 0.834″.  相似文献   

20.
正Artemia cysts are an extremely important component of aquaculture diets.It is well established that the cultivation of fish and shellfish derive substantial health and growth advantages when Artemia are included in the diets of the  相似文献   

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