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贺兰山孔兹岩系的变质时代及其对华北克拉通西部陆块演化的制约 被引量:58
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作者 周喜文 耿元生 《岩石学报》 SCIE EI CAS CSCD 北大核心 2009年第8期1843-1852,共10页
贺兰山孔兹岩系作为华北克拉通西部孔兹岩带的重要组成部分,其变质时代问题一直悬而未决。利用SHRIMP锆石U-Pb定年技术,对贺兰山孔兹岩系中3个代表性富铝片麻岩(石榴堇青钾长片麻岩、石榴堇青二长片麻岩与石榴黑云斜长片麻岩)样品进行... 贺兰山孔兹岩系作为华北克拉通西部孔兹岩带的重要组成部分,其变质时代问题一直悬而未决。利用SHRIMP锆石U-Pb定年技术,对贺兰山孔兹岩系中3个代表性富铝片麻岩(石榴堇青钾长片麻岩、石榴堇青二长片麻岩与石榴黑云斜长片麻岩)样品进行了精确定年。发现这3种岩石虽处不同层位,但其碎屑锆石年龄却非常集中,各测点^(207)Pb/^(206)Pb年龄总体变化在2.0~2.1Ga之间,加权平均年龄则在2017~2040Ma之间。这些碎屑锆石都具有岩浆结构特征,反映当时曾存在大规模花岗质岩浆活动,所成岩体为孔兹岩系沉积提供了充足物源。另有少量大于2.5Ga的碎屑锆石(2520~2949Ma),表明本区存在太古代岩浆活动记录。本区石榴堇青二长片麻岩中发育典型的变质增生锆石,其成因很可能与黑云母的脱水熔融反应有关。利用该锆石确定贺兰山孔兹岩系的变质时代为1950±8Ma。该时代与东部大青山、乌拉山孔兹岩系变质时代相同,表明华北克拉通西部的阴山地块与鄂尔多斯地块大体是以平行的方式正面拼贴到一起的。 展开更多
关键词 贺兰山 孔兹岩系 变质时代 华北克拉通 演化 region KHONDALITE series metamorphic age North China Craton 黑云斜长片麻岩 碎屑锆石年龄 岩浆活动 石榴 magmatic origin 鄂尔多斯地块 time SHRIMP ages Ordos block 富铝片麻岩
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内蒙古贺兰山地区古元古代晚期的花岗岩浆事件及其地质意义:同位素年代学的证据 被引量:50
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作者 耿元生 周喜文 +1 位作者 王新社 任留东 《岩石学报》 SCIE EI CAS CSCD 北大核心 2009年第8期1830-1842,共13页
位于华北克拉通西缘的贺兰山杂岩主要由孔兹岩系和变形花岗岩(正片麻岩)所组成,前者主要由夕线石榴片麻岩、石榴二长片麻岩、变粒岩和少量的大理岩及麻粒岩所组成,后者主要包括黑云斜长片麻岩、石榴子石花岗岩、斑状花岗岩和片麻状变质... 位于华北克拉通西缘的贺兰山杂岩主要由孔兹岩系和变形花岗岩(正片麻岩)所组成,前者主要由夕线石榴片麻岩、石榴二长片麻岩、变粒岩和少量的大理岩及麻粒岩所组成,后者主要包括黑云斜长片麻岩、石榴子石花岗岩、斑状花岗岩和片麻状变质闪长岩。本文报道了该区变形花岗岩的锆石SHRIMP U-Pb定年结果。黑云二长片麻岩和石榴子石花岗岩分别形成于2053±58Ma和2047±42Ma,斑状花岗岩和片麻状闪长岩分别在1955Ma和1920Ma侵位。大量的年代学资料表明,在华北克拉通北缘存在一条古元古代晚期的花岗杂岩带,该带中的花岗杂岩主要形成于三个阶段,第一阶段大于2.0Ga,第二阶段主要出现在2.0~1.87Ga期间,第三阶段的花岗杂岩在1.85~1.80Ga期间侵位。年代学研究还表明,古元古代晚期的花岗岩浆作用常常与变质事件紧密相关。 展开更多
关键词 内蒙古 贺兰山地区 古代晚期 岩浆事件 地质意义 同位素年代学 证据 area North China Craton 变形花岗岩 黑云斜长片麻岩 花岗杂岩 regional metamorphism 华北克拉通北缘 stage 石榴子石 黑云二长片麻岩 zircon SHRIMP 闪长岩 片麻状
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桐柏地区高压变质地体在地壳中的抬升机制 被引量:21
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作者 崔建军 胡健民 刘晓春 《岩石学报》 SCIE EI CAS CSCD 北大核心 2009年第9期2165-2176,共12页
桐柏杂岩位于秦岭与大别造山带之间,南北两侧为NWW-SEE向延伸的含榴辉岩高压变质地体,其构造就位过程及其与高压变质地体的构造关系为地质学家们所关注。本文研究表明,所谓的桐柏杂岩实际上是一个早白垩世花岗质片麻岩杂岩体,其内包裹... 桐柏杂岩位于秦岭与大别造山带之间,南北两侧为NWW-SEE向延伸的含榴辉岩高压变质地体,其构造就位过程及其与高压变质地体的构造关系为地质学家们所关注。本文研究表明,所谓的桐柏杂岩实际上是一个早白垩世花岗质片麻岩杂岩体,其内包裹一定数量的三叠纪中高级变质岩石。桐柏杂岩南北两条边界韧性剪切带具有相反的运动学指向,分别为大型右行和左行韧性剪切带,其形成时代为131Ma。这两条韧性剪切带中的剪切面理分别朝SSW和NNE向倾斜,韧性剪切带及杂岩体内部发育的拉伸线理均稳定地朝SEE方向缓倾伏。而在杂岩体的东端发育低角度近南北向韧性剪切变形带,其糜棱面理朝SEE方向低角度缓倾斜,矿物拉伸线理也朝SEE方向低角度缓倾伏,运动学标志指示东侧地质体朝295°~310°的方向逆冲。因此,桐柏杂岩实际上被一个顺造山带的韧性剪切带所围限,这个韧性剪切带及杂岩体内部韧性变形运动学指示了一个早白垩世由东向西的低角度抬升过程,而这一过程直接导致了含榴辉岩高压变质地体沿着造山带的方向从地壳深部抬升到近地表。这一研究结果对理解和认识桐柏-大别-苏鲁地区高压-超高压变质地体的晚期抬升过程具有重要意义。 展开更多
关键词 桐柏地区 高压 变质地体 壳中 抬升机制 area levels China Tongbai complex 韧性剪切带 DUCTILE SHEAR zone METAMORPHIC rocks SHEAR zones 桐柏杂岩 Early CRETACEOUS 杂岩体 低角度 southern SEE northern
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东南极普里兹带多斯变质作用及其对罗迪尼亚和冈瓦纳超大陆重建的启示 被引量:9
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作者 刘晓春 《岩石学报》 SCIE EI CAS CSCD 北大核心 2009年第8期1808-1818,共11页
东南极普里兹带是一条经受格林维尔期和泛非期高级构造热事件影响的多相变质带,其构造演化过程与罗迪尼亚和冈瓦纳超大陆的形成密切相关。新的岩石学和年代学资料表明,普里兹带中的格林维尔期高级变质作用是区域性的,并经历了>970Ma... 东南极普里兹带是一条经受格林维尔期和泛非期高级构造热事件影响的多相变质带,其构造演化过程与罗迪尼亚和冈瓦纳超大陆的形成密切相关。新的岩石学和年代学资料表明,普里兹带中的格林维尔期高级变质作用是区域性的,并经历了>970Ma和930~900Ma两个演化阶段(期),变质条件达到相对高温高压的麻粒岩相。格林维尔期造山作用起始于活动大陆边缘或岛弧环境下的岩浆增生,最后发展到陆陆碰撞,从而使印度、东南极西陆块和非洲的卡拉哈里克拉通拼合在一起,构成了罗迪尼亚超大陆的重要组成部分之一。普里兹带中的泛非期高级变质作用并不象前人认为的那样只发生在中低压麻粒岩相条件下,而是达到高压麻粒岩相,并具有近等温减压的顺时针P-T演化轨迹。格林维尔期变质先驱的普遍存在说明泛非期碰撞造山事件主要叠加在印度-南极陆块东缘的基底杂岩之上,所以其主缝合线的位置应该在现今普里兹带的东南方向,并可能向南极内陆延伸到甘布尔采夫冰下山脉。对不同类型岩石的精细定年揭示,普里兹带中泛非期造山作用过程从570Ma一直持续到490Ma,这与东非造山带的晚期碰撞阶段大致相吻合。因此,冈瓦纳超大陆的最后拼合可能是通过西冈瓦纳、印度-南极陆块和澳大利亚-南极陆块等三个陆块的近于同期碰撞来完成的。 展开更多
关键词 东南极 普里兹带 高级变质作用 罗迪尼亚超大陆 冈瓦纳 超大陆重建 启示 East Antarctica GRANULITE facies active continental margin 麻粒岩相 泛非期 tectonic evolution 造山作用 碰撞造山事件 HIGH temperature HIGH pressure 印度 活动大陆边缘 during
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变质作用分类的历史回顾和新的试行分类雏议 被引量:4
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作者 沈其韩 耿元生 《岩石学报》 SCIE EI CAS CSCD 北大核心 2009年第8期1737-1748,共12页
根据变质作用分类研究的历史回顾和最新进展,本文介绍了一个试行的、较系统的变质作用分类方案,可分为局部性的变质作用和区域性的变质作用两个大类9个类型。局部性的变质作用包括以下5个类型:(1)接触变质作用,包括热变质作用、接触交... 根据变质作用分类研究的历史回顾和最新进展,本文介绍了一个试行的、较系统的变质作用分类方案,可分为局部性的变质作用和区域性的变质作用两个大类9个类型。局部性的变质作用包括以下5个类型:(1)接触变质作用,包括热变质作用、接触交代变质作用和高热变质作用3个亚类;(2)低-中-高温动力变质作用,包括低-中-高温韧性剪切带变质作用和温压递进逆冲断层变质作用2个亚类;(3)冲击变质作用;(4)水热变质作用;(5)燃烧变质作用。区域性的变质作用可分为以下4个类型;(6)早前寒武纪克拉通基底变质作用-低中压-中高温区域变质作用,可分为5个亚类,分别是低-中压角闪岩相变质作用、低-中压麻粒岩相变质作用、低-中压角闪岩相-麻粒岩相变质作用、低-中压绿片岩相-角闪岩相递增的变质作用和区域超高温麻粒岩相变质作用;(7)造山带变质作用,可分为3个亚类,分别是低温-低压区域动力变质作用、碰撞造山变质作用和深俯冲高压-超高压区域变质作用;(8)埋深变质作用;(9)洋底变质作用。 展开更多
关键词 热变质作用 作用分类 历史回顾 雏议 systematic classification granulite facies METAMORPHISM regional METAMORPHISM 中高温区域变质作用 麻粒岩相 角闪岩相变质作用 动力变质作用 ductile shear ZONE 亚类 subduction ZONE dynamic 区域性 局部性 接触变质作用 冲击变质作用 早前寒武纪
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Single-zircon dating of Precambrian strata in the west sector of the northern Qilian Mountains and its geological significance 被引量:8
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作者 Jingwen Mao Zhaochong Zhang +3 位作者 Jianmin Yang Biao Song Maobing Wu Guochao Zuo 《Chinese Science Bulletin》 SCIE EI CAS 1998年第15期1289-1294,共6页
Single_zircon evaporation method was employed in the present study to determine the age of the iron_bearing rock series in Precambrian strata in the western sector of the northern Qilian Mountains. Three zircon ages f... Single_zircon evaporation method was employed in the present study to determine the age of the iron_bearing rock series in Precambrian strata in the western sector of the northern Qilian Mountains. Three zircon ages from the diabase of the Aoyougou ophiolite previously put into Upper Lithologic Formation of the Zhulongguan Group are (1 840±2), (1 783±2) and (1 784±2) Ma respectively, whereas the zircon ages from the welded breccias in the Zhulongguan Group are (733±7), (738±4) and (604±6) Ma respectively. These results show that they should belong to the bottom of the middle Proterozoic and the upper part of upper Proterozoic respectively. 展开更多
关键词 single_zircon DATING PROTEROZOIC STRATIGRAPHIC division.
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Discovery of granulite from the Fuping area in southern Qinling Mountains and its geological significance 被引量:6
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作者 Chunjing Wei Chonghui Yang +1 位作者 Shouguang Zhang Rongshe Li 《Chinese Science Bulletin》 SCIE EI CAS 1998年第16期1358-1362,共4页
Two-pyroxene-bearing granulites were discovered for the first time in the Hercynian-Indosinian metamorphic belt of the southern Qinling Mountains. The granulites occur in the lower part of the Fuping complex and are d... Two-pyroxene-bearing granulites were discovered for the first time in the Hercynian-Indosinian metamorphic belt of the southern Qinling Mountains. The granulites occur in the lower part of the Fuping complex and are dominated by intermediate-acidic rocks intercalated with a small amount of bands and lenses of basic granulites. The main metamorphic minerals include orthopyroxene, clinopyroxene, biotite, plagioclase and quartz, and orthopyroxenes are often retrogressively transformed into amphiboles. The metamorphic conditions have been estimated to be %T%=720-780℃ and %P%=0.6 GPa. The granulite-bearing Fuping complex probably belongs to early Proterozoic in age. Whether it occurs as the crystalline basement of the southern Qinling Hercynian-Indosinian orogenic belt or as a thrusted slice in the collisional process needs further study. 展开更多
关键词 GRANULITE Fuping complex QINLING OROGENIC belt.
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The ages of U-Pb and Sm-Nd for eclogite from the western segment of Altyn Tagh tectonic belt——Evidence for existence of Caledonian orogenic root 被引量:47
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作者 Jianxin Zhang Zeming Zhang +2 位作者 Zhiqin Xu Jingsui Yang Junwen Cui 《Chinese Science Bulletin》 SCIE EI CAS 1999年第24期2256-2259,共4页
The eclogites of Altyn Tagh tectonic belt occur as lens within gneisses characterized by amphibolite-facies mineral parageneses. The well-preserved eclogite is selected for Sm-Nd and U-Pb isotopic dating. The Sm-Nd is... The eclogites of Altyn Tagh tectonic belt occur as lens within gneisses characterized by amphibolite-facies mineral parageneses. The well-preserved eclogite is selected for Sm-Nd and U-Pb isotopic dating. The Sm-Nd isotopic data yield a whole rock-garnet-omphacite isochron of (500 ?10) Ma. The U-Pb isotopic measurements of zircons show that the four 展开更多
关键词 Altyn Tagh TECTONIC BELT ECLOGITE SM-ND DATING U-PB dating.
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Earthquake events in Neoproterozoic and Early Paleozoic and its relationship with supercontinental Rodinia in North China 被引量:26
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作者 Xiufu Qiao Linzhi Gao 《Chinese Science Bulletin》 SCIE EI CAS 2000年第10期931-935,共5页
Carbonate liquefied veins in limestone and liquefied mud veins in mudstone are the result by earthquake, which is liquefied in sediments and a strong earthquake event remains clearly records in strata. 24 strata units... Carbonate liquefied veins in limestone and liquefied mud veins in mudstone are the result by earthquake, which is liquefied in sediments and a strong earthquake event remains clearly records in strata. 24 strata units with earthquake events (molar tooth), which are subdivided into 11 seismic periods, have been distinguished from Mid-Proterozoic to Early Paleozoic strata in the Sino-Korean platform. The distributions of them represent paleo-seismic tectonic zones in different periods, which is tallied with convergent continental block before Proterozoic supercontinental Rodinia and the evidence of the breakup or splitting developed in the inner Sino-Korean Platform in 700 Ma. 展开更多
关键词 SEISMITES CARBONATE liquefied VEINS paleo-Tanlu zone rodinia.
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Evidence for UHP metamor-phism of eclogites from the Altun Mountains 被引量:33
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作者 Jianxin Zhang Jingsui Yang +3 位作者 Zhiqin Xu Fancong Meng Haibing Li Rendeng Shi 《Chinese Science Bulletin》 SCIE EI CAS 2002年第9期751-755,共5页
Ultrahigh pressure (UHP) metamorphism refers to metamorphism that has occurred at pressures for the stability of coesite. The polycrystalline quartz inclusions showing the characteristic texture within garnets of eclo... Ultrahigh pressure (UHP) metamorphism refers to metamorphism that has occurred at pressures for the stability of coesite. The polycrystalline quartz inclusions showing the characteristic texture within garnets of eclogites indicates the pre-existence of coesites under the peak meta-morphic condition. The unusual exsolution textures in om-pacites and apatites, and the pressure estimations of phengite-bearing eclogites have been taken to provide further proof of eclogite formation under the UHP conditions. Combined with the fact that coesites have been observed in country rocks of eclogites in North Qaidam Mountains, another UHP metamorphic belt cut by the large-scale strike-slip fault in the Altun-North Qaidam area of China is confirmed. 展开更多
关键词 Altun MOUNTAINS ECLOGITE UHP metamorphism.
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Experimental observation of deep crust fluid-NaCl aqueous solution at elevated temperatures and pressures and its significance 被引量:14
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作者 Ronghua Zhang Shumin Hu 《Chinese Science Bulletin》 SCIE EI CAS 1999年第7期654-660,共7页
In order to reveal the nature of deep crust fluids, the phase relations of NaCI-saturated solution at high temperatures and pressures in a hydrothermal diamond anvil cell (HDAC)are investigated. Salinity of the soluti... In order to reveal the nature of deep crust fluids, the phase relations of NaCI-saturated solution at high temperatures and pressures in a hydrothermal diamond anvil cell (HDAC)are investigated. Salinity of the solutions observed is about 35%—50%. The temperatures for the observation range from 25 to 850℃ and the pressures from 1 atm to about 1 GPa. A supercritical single phase, liquid phase (L), vapor phase (V), solid phase (H), L + H, H + V + L and the near-critical phases L + V can be observed. A two-phase (L + V) immiscibility field for the NaCI solution has been discovered to lie in a wide range of temperatures and pressures:from 250( ± 3) to 721℃. Within this field there are two parts, where the upper high temperature part of the two-phase regions is very unstable in character. It is possible to observe a 'critical phenomenon'. In some of our experiments an 'explosion' almost constantly occurred at the interface between the liquid and vapor phases, making the interface obscure, and a 展开更多
关键词 TWO-PHASE IMMISCIBILITY CRITICAL phenomenon solution structure.
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Stable carbon and oxygen isotopic compositions of carbonates in middle Mesoproterozoic Wumishan Formation and sea-level change 被引量:8
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作者 Renwei Li Jinshi Chen Shukun Zhang 《Chinese Science Bulletin》 SCIE EI CAS 1999年第23期2130-2136,共7页
δ13C of dolostones from the Wumishan Formation (1 310-1 207 Ma) in the Ming Tombs area near Beijing ranges from - 1.5 to 1.5‰ (PDB), and generally, the δ18O ranges from - 4 to - 5‰ (PDB). The secular variation of ... δ13C of dolostones from the Wumishan Formation (1 310-1 207 Ma) in the Ming Tombs area near Beijing ranges from - 1.5 to 1.5‰ (PDB), and generally, the δ18O ranges from - 4 to - 5‰ (PDB). The secular variation of stable carbon isotopic compositions is cyclic. δ13C displays positive shifts from a sequence boundary to 1.5 per mil (PDB), then 展开更多
关键词 carbon and OXYGEN ISOTOPES Mesoproterozoic. SEA-LEVEL change.
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Relationship between polymetallic nodules and submarine hydrothermalism in the Central Pacific Ocean 被引量:4
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作者 Li, YH Song, HB +1 位作者 Li, JC Yao, XM 《Chinese Science Bulletin》 SCIE EI CAS 1997年第23期1980-1983,共4页
THE huge reserves of submarine polymetallic nodules make them an important kind of potentialmineral resources. It has already been discovered that polymetallic nodules are related withsubmarine vollcanogene hydrotherm... THE huge reserves of submarine polymetallic nodules make them an important kind of potentialmineral resources. It has already been discovered that polymetallic nodules are related withsubmarine vollcanogene hydrothermalism. For example, pyroclasts usually occur as coresubstances of the nodules, and large amounts of mineralizing materials such as manganese aredischarged to form ferromanganese oxides along with the submarine vocanogene hydrothermal- 展开更多
关键词 POLYMETALLIC NODULES SUBMARINE hydrothermalism HELIUM isotope.
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A finite-element simulation on deformational energy in structural deformed zone 被引量:3
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作者 Guxian Lü Hongcai Wang +3 位作者 Weizhen Peng Xiaobo Li Tao Guo Chusun Guo 《Chinese Science Bulletin》 SCIE EI CAS 1999年第11期1053-1056,共4页
Under the same conditions of external force, simulations on differences of deformational energy in structural zones, which have different deformational behavior, and that on the distribution of the differences have be... Under the same conditions of external force, simulations on differences of deformational energy in structural zones, which have different deformational behavior, and that on the distribution of the differences have been carried out by means of finite-element method. Shear deformational energy U_w is higher than volume deformational energy U_T by about one order of magnitude, and deformationat energy U_B( = U_w + U_T) and U_w show a trend to be larger→largest→small in quantity in structural zones of different deformational properties, which correspond to compressive, shear, tensile zones, respectively, but U_T shows a trend to be large→small gradually. This has a considerable significance in the study of tectonic heat and mineral liquid migration in association with the research on tectonic additional hydrostatic pressure. 展开更多
关键词 STRUCTURAL deformational ZONE ELASTIC deformational ENERGY FINITE-ELEMENT method.
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The first discovery of eclogite and Palaeoproterozoic granitoids in the Beishan area,northwestern Gansu Province,China 被引量:2
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作者 Hualin Mei Haifeng Yu +6 位作者 Quan Li Songnian Lu Huimin Li Yicheng Zuo Guochao Zuo Dejin Ye Jincheng Liu 《Chinese Science Bulletin》 SCIE EI CAS 1999年第4期356-361,共6页
The eclogite, discovered in Liuyuan, occurs as lenticular enclave within granitic gneiss. It has typical features of eclogite in petrology and mineralogy. The eclogite provides an important wirdow to reconstruct the t... The eclogite, discovered in Liuyuan, occurs as lenticular enclave within granitic gneiss. It has typical features of eclogite in petrology and mineralogy. The eclogite provides an important wirdow to reconstruct the tectonic border of the Tarim block. The granitoids, located in Baihu area, yield U-Pb zircon ages of 1 660—2 000 Ma (Palaeoproterozoic), which irrplies an early Precambrian basement in the area. 展开更多
关键词 ECLOGITE PALAEOPROTEROZOIC GRANITOIDS Beishan area GANSU Province.
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The variety of thermal conduction resulting from segmented degree of heat source body and its bearing on temperature change 被引量:1
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作者 Guxian Lü Hongcai Wang +2 位作者 Tao Guo Yinsheng Ma Daogong Hu 《Chinese Science Bulletin》 SCIE EI CAS 1999年第15期1411-1415,共5页
The differences of thermal conduction and its temperature-varying track of the heat source body at various structural environments have been studied. Hypothetically, geologic heat source body is cut successively into ... The differences of thermal conduction and its temperature-varying track of the heat source body at various structural environments have been studied. Hypothetically, geologic heat source body is cut successively into several segregative bodies with a fixed cubage. With the segmented number increasing, the conductive surface area of heat source body begins to get larger, which separately is similar to the heat geologic body in different tectonic zones that has a various enclosed coefficient η(η=S<sub>0</sub>/sum from i=(1,n)(S<sub>i</sub>)). Finite-element simulation result shows that the thermal conduction speed of spreading from the heat source body to its wall rock is slow→higher→highest, when heat source bodies are situated respectively at compressive, shear and tensile deformation zones, corresponding rates of their temperature drop are low→higher→highest. Research indicates that the temperature’s dropping rate of heat source body has an inverse relationship with enclosed coefficient η for different structural 展开更多
关键词 thermal conduction SEGMENTED DEGREE FINITE-ELEMENT tectono-physicochemistry.
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Helium isotopic study on mantle degassing in the Altay orogenic zone,China
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作者 Denghong Wang Yuchuan Chen +2 位作者 Zhigang Xu Hongyang Li Tiande Li 《Chinese Science Bulletin》 SCIE EI CAS 1999年第11期1050-1053,共4页
New helium isotopic data of ores and rocks from the Altay orogenic zone, Xinjiang,China are reported, which show that the pegmatites from No. 3 vein in the Keketuohai area have high <sup>3</sup>He/<sup&... New helium isotopic data of ores and rocks from the Altay orogenic zone, Xinjiang,China are reported, which show that the pegmatites from No. 3 vein in the Keketuohai area have high <sup>3</sup>He/<sup>4</sup>He ratios up to 1 .795 x 10<sup>-6</sup> and 2.54 x 10<sup>-6</sup>. Such a result suggests that the metallogenic process of rare metal deposits in the Altay orogenic zone might be related to mantle degassing. 展开更多
关键词 OROGENIC ZONE MANTLE DEGASSING HELIUM isotope.
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Discovery of eclogite at northern margin of Qaidam Basin,NW China 被引量:36
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作者 Jingsui Yang Zhiqin Xu +4 位作者 Haibing Li Cailai Wu Junwen Cui Jianxin Zhang Wen Chen 《Chinese Science Bulletin》 SCIE EI CAS 1998年第20期1755-1760,共6页
Eclogite was first discovered at the northern margin of the Qaidam Basin in this study. It occurs as pods in the gneiss sequence of Middle to Upper Proterozoic age and is mainly composed of garnet, omphacite, phengite... Eclogite was first discovered at the northern margin of the Qaidam Basin in this study. It occurs as pods in the gneiss sequence of Middle to Upper Proterozoic age and is mainly composed of garnet, omphacite, phengite and rutile. The garnets contain 44%-62% of almandine, 15%-33% of grossular and 12%-30% of pyrope molecules, and the omphacites contain 40%-46% of jadeite. Applying garnet_clinopyroxene thermometry and jadeite geobarometry, the peak conditions of eclogite facies metamorphism occurred at about (722±123)℃ and at the pressure of up to c. 22 ×10 8 Pa. 展开更多
关键词 ECLOGITE high_pressure METAMORPHISM Da Qaidam Qinghai_Xizang Plateau.
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Structural OH in mantle-derived clinopyroxene megacrysts from Nushan 被引量:6
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作者 Qunke Xia Daogong Chen Lihe Guo 《Chinese Science Bulletin》 SCIE EI CAS 1998年第20期1742-1745,共4页
Thirteen clinopyroxene megacrysts from Nushan Cenozoic basalts have been investigated by Fourier transform infrared spectrometer(FTIR). The results demonstrate that all samples contain trace amount of structural OH. C... Thirteen clinopyroxene megacrysts from Nushan Cenozoic basalts have been investigated by Fourier transform infrared spectrometer(FTIR). The results demonstrate that all samples contain trace amount of structural OH. Clinopyroxenes from Nushan show four groups of absorption bands, in which, 3 472-3 506 cm -1 is the major characteristic one. It is suggested that the position of major band is probably related to Al content: the position of major characteristic band for high_Al samples is around 3 470 cm -1 , whereas that for low_Al samples around 3 620 cm -1 . 展开更多
关键词 STRUCTURAL OH CLINOPYROXENE Nushan.
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