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1.
雷州英峰岭玄武岩中单斜辉石巨晶的地球化学和地幔交代作用 总被引:5,自引:1,他引:5
雷州半岛英峰岭火山岩中单斜辉石巨晶以低Mg^#值(0.62—0.47)、贫重稀土(HREE)和富Al2O3、TiO2、Na2O和中稀土(MREE)为特征,并具有明显的成分变化。随着Mg^#降低,单斜辉石的Al:O,(11.58~6.97%,)、TiO,(2.28~1.06%)和HREE逐渐降低。这种变化特征不同于世界上大多数辉石巨晶的变化规律。随着演化辉石巨晶的大多数不相容元素,如Nb、Sr、Zr、Hf和LREE—MREE逐渐增加。低的Mg^#值和Ni、Co、Cr含量指示巨晶母岩浆是一种强烈演化的残余岩浆(Mg^#=0.27~0.35)。分离结晶模拟表明本研究最富镁的巨晶(Lz-54)的母岩浆很可能是由拉斑玄武质岩浆经70~80%,以单斜辉石为主的结晶分异后形成。而本研究的其它辉石巨晶是该母岩浆在不同演化阶段(25~80%)分离结晶的产物。分离矿物中除了单斜辉石还包含了大量的石榴子石、斜长石和钛铁矿。温压计算表明英峰岭巨晶是高温岩浆在56~60km深的上地幔的结晶产物(r=1290℃~1130℃,P=1.73~1.83GPa),这一深度有利于石榴子石结晶。对比不同地区辉石巨晶的成分特征和形成条件,作者指出不同地区单斜辉石巨晶各种元素的不同变化规律主要受母岩浆成分和结晶条件控制。巨晶母岩浆在地幔结晶时对围岩橄榄岩进行了不同程度的交代作用。早期贫流体的岩浆对橄榄岩的交代作用较弱,只有Sr,La等强活动性元素被明显改变;晚期富流体(F,P,H2O)岩浆对橄榄岩的交代作用强烈,大多数元素被明显改变。因此,可以推断交代熔体中流体的含量是影响地幔橄榄岩交代作用的关键。 相似文献
2.
地幔橄榄岩部分熔融及相转变(尖晶石相→斜长石相)过程中的固相化学成分演化──Ⅰ.实验研究 总被引:1,自引:0,他引:1
在温度为ll30─l450℃,压力为0.4─2.0GPa条件下,实验研究了地幔橄榄岩部分熔融及相转变(尖晶石相→斜长石相)过程中的固相化学成分演变。在部分熔融中,随熔融度的增大,橄榄石的Mg/(Mg+Fe)尖晶石和斜方辉石的Mg/(Mg+Fe)及Cr/(Cr+Al)逐渐增大;而橄榄石中的Ca含量增至单斜辉石消失后逐渐降低;尖晶石中的Ti以较低的含量(TiO2<0.15%)保持不变或稍有降低;斜方辉石中的Ti含量及单斜辉石的Na和Ti含量逐渐降低,直至非常小的值。在从尖晶石橄榄岩向斜长石橄榄岩的相转变过程中,尖晶石强烈富Ti,且其Cr/(Cr+Al)逐渐增大;斜方辉石中的Ti含量和Cr/(Cr+Al)同时逐渐增大;单斜辉石中的Na含量降低而Ti含量升高或保持不变。当斜长石橄榄岩经受了部分熔融(即使很微弱),其在相转变过程中引起的各矿物相的化学成分特征要全部消失,而表现部分熔融作用的特征。这可作为判别橄榄岩在斜长石相域内是否经历了部分熔融的标志。关键词 相似文献
3.
陆下和洋底脊橄榄岩单斜辉石中的Na.Al^IV和Al^VI:地幔中不同熔融… 总被引:1,自引:0,他引:1
把从大西洋洋中脊采集的无斜长石的尖晶石二辉橄缆岩和方辉橄缆岩中的单斜辉石的Na-Al^IV和Al^VI浓度与陆下和前大洋的无斜长石的尖晶石橄榄岩的数据进行了比较。单斜辉石的Al2O3含量在洋底橄缆岩组和陆下橄缆岩组中的同一范围内发生变化,从高铝至贫铝。然而,洋底橄缆岩中单斜辉石的Na含量(0.02 ̄0.6wt%Na2O)和Al^VI/Al^IV比值(0.3 ̄1)都低于陆下橄缆岩单斜辉石的Na含量( 相似文献
4.
在温度为1130-1450℃,压力为0.4-2.0GPa条件下,实验研究了地幔橄榄岩部分熔融及相转变(尖晶石相→斜长石相)过程中的固相化学成分演变。在部分熔融中,随熔融度的增大,橄榄石的Mg/(Mg+Fe)^尖晶石和斜方辉石的Mg/(Mg+Fe)及Cr/(Cr+Al)逐渐增大;而橄榄石中的Ca含量增至单斜辉石消失后逐渐降低;尖晶石中的Ti以较低的含量(TiO2〈0.15%)保持不变或稍有降低;斜方 相似文献
5.
辽西阜新中生代玄武岩中深源捕虏体的岩石学和矿物化学研究 总被引:16,自引:3,他引:13
辽西阜新中生代碱性玄武岩的K-Ar同位素年龄为84.76±1.67Ma, 其中含有丰富的深源岩石捕虏体, 包括角闪尖晶二辉橄榄岩、尖晶石二辉橄榄岩、含长角闪二辉石岩、二辉麻粒岩和辉石斜长片麻岩等。与新生代玄武岩中的同类捕虏体相比, 橄榄岩类捕虏体中橄榄石的成分相似 (Fo= 86~91), 透辉石具有富Al、贫Cr 和Ca 的特点, 尖晶石的成分以MgAl2 O4 为主, 有的橄榄岩捕虏体中含少量韭闪石。二辉麻粒岩捕虏体中的斜方辉石为紫苏辉石, 单斜辉石为普通辉石, 斜长石属于更长石。橄榄岩类捕虏体的平衡温度为1012.6℃~1272.1℃; 压力为1.825~2.935GPa, 二辉麻粒岩和片麻岩的平衡温度为892℃~1157℃。该类深源岩石捕虏体的发现对中国东部中生代上地幔和下地壳的研究均具有重要意义。 相似文献
6.
分析了全球一些有代表性的上地幔尖晶石橄榄岩和斜长石橄榄岩中各矿物的化学成分变化特征。发现在斜长石橄榄岩中,尖晶石和斜方辉石富Ti,且Ti含量随Cr/(Cr+Al)的增大而增大;单斜辉石富Ti贫Na,其Ti含量随Na含量的增大而减少。据此,结合实验结果,可以肯定世界各地大多数斜长石二辉橄榄岩在斜长石相域内未经受部分熔融。岩体所曾经受的部分熔融只发生在尖晶石或石榴石相。它们的相对熔融度可以用下面两个指标来估计:(1)最贫Ti尖晶石的Cr/(Cr+Al);(2)单斜辉石的最高Na含量。对于尖晶石橄榄岩,从二辉橄榄岩、方辉橄榄岩到纯橄榄岩,其尖晶石和斜方辉石的Cr/(Cr+Al)逐渐增大,而含量很低的Ti或Na在尖晶石、斜方辉石及单斜辉石中保持不变或趋向逐渐减小。尖晶石橄榄岩的相对熔融度可据尖晶石的Cr/(Cr+Al)和单斜辉石的Na含量来判断。 相似文献
7.
为探讨扬子克拉通古元古代变质作用特征及其形成的构造背景,对黄陵穹窿北部石榴斜长角闪岩开展了岩相学、地球化学和年代学研究。结果表明,石榴斜长角闪岩中主要矿物有石榴子石、斜长石、角闪石、单斜辉石、石英、钛铁矿等,其中保留有3个阶段的不同变质期次的矿物组合,进变质矿物组合为角闪石+斜长石+石英+钛铁矿,峰期矿物组合为石榴子石+角闪石+斜长石+单斜辉石+石英+钛铁矿,退变质矿物组合为石榴子石+角闪石+斜长石+石英+钛铁矿。石榴斜长角闪岩原岩为亚碱性玄武岩,属于拉斑系列,Mg#较低,表明其原岩经历了一定程度的分异作用。使用传统地质温压计计算不同变质阶段的温压条件分别为:进变质阶段,t=596~625℃,p=0.70~0.82 GPa;峰期变质阶段,t≈760℃,p≈1.35 GPa;退变质阶段,t=692~738℃,p=0.68~0.74 GPa,并建立了一条顺时针的p-t轨迹,显示出先升温升压至峰期阶段,随后发生近等温减压的过程。这一p-t轨迹体现了汇聚板块边缘俯冲-碰撞的构造背景,对石榴斜长角闪岩中的锆石进行U-Pb定年,获得了2 008±11 Ma的谐和年龄,并结合该... 相似文献
8.
通常认为基性岩中辉石巨晶及堆晶是基性岩浆在中高压条件下的结晶产物 ,所以辉石巨晶及堆晶被视为深部地质作用的信息载体。中国东部新生代玄武岩中辉石巨晶、堆晶及地幔捕虏晶的发现与研究仅局限于沿海数省 ,武夷山西部江西未见报道 ;而中生代玄武岩中辉石巨晶、堆晶发现与研究在整个华南仍是一个空白。笔者近年来在江西广丰白垩纪红盆地工作时 ,于中生代玄武岩和新生代基性岩脉中分别发现了单斜辉石巨晶 (堆晶 )。中生代玄武岩以层状夹层产于早白垩世周田组地层中 ,K -Ar年龄为 98.8Ma ,1 0 0Ma和 1 0 4Ma。玄武岩中单斜辉石巨晶… 相似文献
9.
黄山东镁铁超镁铁杂岩中的辉石化学成分研究 总被引:7,自引:0,他引:7
通过对黄山东镁铁超镁铁杂岩的辉石化学成分研究,证明辉石的化学成分受寄主岩石类型的制约,从超镁铁岩相到角闪辉长岩相斜方辉石的化学成分由富MgO、SiO_2、Al_2O_3、Cr_2O_3到富FeO、TiO_2、CaO、MnO;单斜辉石化学成分由富Al_2O_3、Cr_2O_3、Na_2O、MgO到富FeO、MnO、CoO。在同一寄主岩石中,单斜辉石比斜方辉石富TiO_2、Al_2O_3、Cr_2O_3、CaO和Na_2O,贫MgO、SiO_2、MnO和FeO。根据辉石化学成分特征得出黄山东杂岩形成于岛弧环境,为上地幔石榴二辉檄榄岩部分熔融形成的拉斑玄武岩岩浆结晶分异作用的产物。 相似文献
10.
11.
Inter-regional correlation of transgressions and regressions in the Cretaceous period 总被引:1,自引:0,他引:1
T. Matsumoto 《Cretaceous Research》1980,1(4):359-373
Well investigated platforms have been selected in each continent, and the history of Cretaceous transgressions and regressions there is concisely reviewed from the available evidence. The factual records have been summarized into a diagram and the timing of the events correlated between distant as well as adjoining areas.On a global scale, major transgressions were stepwise enlarged in space and time from the Neocomian, via Aptian-Albian, to the Late Cretaceous, and the post-Cretaceous regression was very remarkable. Minor cycles of transgression-regression were not always synchronous between different areas. Some of them were, however, nearly synchronous between the areas facing the same ocean.Tectono-eustasy may have been the main cause of the phenomena of transgression-regression, but certain kinds of other tectonic movements which affected even the so-called stable platforms were also responsible for the phenomena. The combined effects of various causes may have been unusual in the Cretaceous, since it was a period of global tectonic activity. The slowing down of this activity followed by readjustments may have been the cause of the global regression at the end of the Cretaceous. 相似文献
12.
The Afyon stratovolcano exhibits lamprophyric rocks, emplaced as hydrovolcanic products, aphanitic lava flows and dyke intrusions, during the final stages of volcanic activity. Most of the Afyon volcanics belong to the silica-saturated alkaline suite, as potassic trachyandesites and trachytes, while the products of the latest activity are lamproitic lamprophyres (jumillite, orendite, verite, fitztroyite) and alkaline lamprophyres (campto-sannaite, sannaite, hyalo-monchiquite, analcime–monchiquite). Afyon lamprophyres exhibit LILE and Zr enrichments, related to mantle metasomatism. 相似文献
13.
K.Naganjaneyulu 《地学前缘(英文版)》2014,5(1):1-2
正The Precambrian shields and associated suture zones of the globe preserve important records of continental growth and destruction,the formation and closure of ocean basins,and the early evolution of the Earth in terms of tectonics,resources,and environment.They also offer critical clues on the nature and style 相似文献
14.
Daniel Harlov 《地学前缘(英文版)》2014,5(5):621-625
正1.Introduction This special issue of Geoscience Frontiers is a tribute volume honoring the life and career of Jacques Touret.A set of research papers has been assembled,which broadly reflect his research interests over his 50 plus year career.These papers focus on the role that fluids play during the formation and evolution of the Earth's crust.Below I provide a brief summary of the life of Jacques Touret,along with a select bibliography of his more important papers.This is then followed by a brief introduction to the papers assembled for this special issue. 相似文献
15.
《地学前缘(英文版)》2014,(1):139-141
正1 AIM AND SCOPE GEOSCIENCE FRONTIERS(GSF)is a bi-monthly international journal that publishes in English high quality original research articles and timely reviews in interdisciplinary fields of Earth and Planetary Sciences.GSF aims to bridge innovative,provocative and challenging concepts and models related to various fields of research including petrology and geochemistry in understanding lithospheric architecture and mantle dynamics,global tectonics,economic geology and fuel exploration,geophysics,stratigraphy and paleontology with new 相似文献
16.
正The world petroleum exploration suggests that,about70%of the world’s potash resources were discovered during oil and gas exploration(Zheng et al.,2007).The Kuqa depression in the Tarim basin is abundant with petroleum exploration data,and 相似文献
17.
正Qarhan Salt Lake is located in the eastern part of the Qaidam Basin,which is first discovered the large potash deposit in the late 1950s.The Bieletan section is located in the west of Qarhan Salt Lake,where saline sediment 相似文献
18.
正With the approach of the 45th World Earth Day,China’s Ministry of Land and Resources issued the status of the Chinese geological survey and environments on 22nd April 2013.Regional geological survey in 2013 achieved new results—(why was oceanic in twice?)polar and oceanic expedition were fully completed,a national census of geography was begun,and 相似文献
19.
正1 Introduction The Lop Nor playa,located in the eastern end of the Tarim Basin,capped with a thick salt crust covering an area of approximately 5,500 km2(Ma 2007)that closely resembles a"Great Ear"in satellite images.Understanding the formation of the salt crust can provide important 相似文献
20.
In Liaoning, Hunan, Guangxi, Guizhou, Gansu, Sichuan, Anhui, Jilin and other provinces in China, there is a wide occurrence of metal quantity over 1000 tons of refractory gold ores, principally because of low gold recoveries and become "stay mine". Features of refi'actory gold ores are: gold in micro-particles or a microscopic state that is wrapped in pyrite, presence of arsenopyrite and other sulfide minerals or disseminated in the crystal lattice of sulfide minerals; harmful impurity elements such as arsenic, carbon, mercury, antimony, copper with high content are closely related with the gold, and these elements affect the contact reaction between the gold and solvent extraction, making the recovery of the gold extraction process low. In the past 20 years, overseas countries have developed the application of the roasting oxidation method, hot acid (alkali) oxidation, bacterial oxidation and flash chlorination oxidation technology to solve this problem.Among these, biological oxidation has developed rapidly in the domestic market and gold enterprises abroad because of its low investment in infrastructure, low production costs, less environmental pollution, simple process and easy control, etc. 相似文献