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11.
Within the high-grade metamorphic basement, the central portion of North China Craton (NCC), a group of Neoarchean khondalites (KS) is identified. They are characterized by large ion lithophile elements (LILE) enrichment, lower abundances of Zr, Hf and Sr. Their rare earth element (REE) distribution has significant LREE enrichment and negative Eu anomalies. The protoliths of KS are interpreted as feldspathic quartzite, shale or pelite and carbonite, deposited in a shallow sea upon cratonic shelf distant from the land. KS's source region might be dominated by granitic rocks, with a minor amount of TTG, underwent comparatively severe chemical weathering. Considering relevent tectonic constraints, we suggest that khondalites from central portion of NCC, an important metamophosed sedimentary cover, are the most significant exogenetic marker of Neoarchean continental cratonization for NCC. 相似文献
12.
卓资孔兹岩系成因矿物学研究 总被引：2，自引：0，他引：2
内蒙古卓资一带孔兹岩系中的辉石、角闪石、石榴石、黑云母均形成于麻粒岩相条件。二辉石地质温度计和石榴石—黑云母地质温度计和压力计计算结果表明,孔兹岩系岩石的变质温度为750—850℃,变质压力为800—920 MPa,变质地温梯度为26.2—28.5℃/km,属中压麻粒岩相。 相似文献
13.
内蒙东南部早前寒武纪孔兹岩系中斜长石的Ca、Na、si、Al“等阳离子存在明显的成分环带。依据其成因机制可划分为生长环带和扩散环带。对不同成因的斜长石环带的成分,采用Ga—Pl—Al_2SiO_5(Sill)—Q压力计,配合Ga—Bi矿物对温度压力计估算,峰期前温度为570～620℃,压力1.0～1.2 GPa;峰期温度为750～850℃,压力0.75～0.85 GPa,峰期后温度为600～650℃,压力为0.5～0.62 GPa。可以确定本区早前寒武纪孔兹岩系变质作用演化为顺时针碰撞造山带型式的P—T—t轨迹。 相似文献
14.
Liu Fulai 《吉林大学学报(地球科学版)》1994,(3)
内蒙卓资出一了大面积太古宙矽线石榴黑云二长片麻岩，其中石榴石的Ｍｇ、〈Ｆｅ〉、Ｍｇ／（Ｍｇ＋Ｆｅ）等呈明显的环带特点。研究表明，石榴石既存在生长环带，也具有扩散环带。其成分环带与石榴石生长过程和变质条件有关。不同成分环带的热力学计算，可以确定变质作用过程中不同阶段的温压条件。 相似文献
15.
LIU Fulai SHEN Qihan Institute of Geology Chinese Academy of Geological Sciences Beijing 《《地质学报》英文版》2003,77(1):28-35
The early Precambrian khondalite series is widely distributed in the Jining-Zhuozi-Fengzhen-Liangcheng area, southeastern Inner Mongolia. The khondalite series mainly consists of sillimanite garnet potash feldspar (or two-feldspar) gneiss and garnet biotite plagioclase gneiss. These gneissic rocks have commonly experienced granulite-facies metamorphism. In zircons separated from sillimanite garnet potash feldspar gneisses, many mineral inclusions, including Sil, Grt, Ky, Kfs, Qtz and Ap, have been identified by the Laser Raman spectroscopy. Generally, prograde metamorphic mineral inclusion assemblages such as Ky + Kfs + Qtz + Ap and Ky + Grt + Kfs + Qtz are preserved in the core of zircon, while peak granulite-facies metamorphic minerals including Sil + Grt + Kfs + Qtz and Sil + Grt + Kfs + Qtz + Ap are identified in the mantle and rim of the same zircon. However, in some zircons are only preserved the peak metamorphic minerals such as Sil + Grt + Kfs + Qtz and Sil + Grt + Kfs + Qtz + Ap from core to ri 相似文献
16.
华北克拉通北缘乌拉山地区发育有大量的古元古代花岗岩,以诺尔音S型花岗岩为代表,本文对诺尔音花岗岩进行详细研究,结果表明:诺尔音花岗岩具有高硅w(Si O_2)=70.03%~75.43%、高铝(w(Al_2O_3)=13.04%~14.87%)、富钾(w(K_2O)=5.36%~6.58%)的特征,其较低的铁镁质量比Mg~#10和较高铝饱和指数A/CNK=1.03~1.21,属于典型的过铝质花岗岩,岩石轻稀土富集,且轻重稀土强烈分馏(La_N/Yb_N=22.3~300.5),配分模式表现为右倾型,具有明显的铕负异常(δEu=0.16~0.55),微量元素原始地幔标准化蛛网图显示,岩石富集K、Rb、Th、Pb,亏损Sr、Ba、Nb、Ta、P、Ti;诺尔音花岗岩与乌拉山地区古元古代孔兹岩系具有相似的主微量地球化学特征,推断其为古元古代阴山陆块与鄂尔多斯陆块碰撞背景下,孔兹岩系深熔作用的产物。LA-ICP-MS锆石U-Pb年龄为(1891±14)Ma和(1863±17)Ma,代表诺尔音S型花岗岩的结晶年龄,与区域内孔兹岩带记录的岩浆-变质事件相吻合。 相似文献
17.
LIU Fulai Institute of Geology Chinese Academy of Geological Sciences Beijing China 《Continental Dynamics》1999,(1)
１．Ｉｎｔｒｏｄｕｃｔｉｏｎ Ｕｐｔｏｎｏｗ,ｍｏｒｅａｎｄｍｏｒｅｇｅｏｌｏｇｉｓｔｓｐｕｔｅｍｐｈａｓｉｓｏｎｔｈｅｆｌｕｉｄｇｅｏｌｏｇｙｏｆｍｅｔａｍｏｒｐｈｉｃｒｏｃｋｓｂｅｃａｕｓｅｆｌｕｉｄｇｅｏｌｏｇｙｉｓａｎｉｍｐｏｒｔａｎｔｗａｙｔｏａｎｉｎｄｅｐｔｈｓｔｕｄｙｏｆｉｎｔｅｒａｃｔｉｏｎｂｅｔｗｅｅｎｆｌｕｉｄｓａｎｄｒｏｃｋｓ．Ｈｏｗｅｖｅｒ,ａｍｏｎｇｍａｎｙｍｅｔｈｏｄｓｔｏｓｔｕｄｙｔｈｅｍｅｔａｍｏｒｐｈｉｃｆｌｕｉｄｓ,ｔｈｅｒｅａｒｅｔｗｏｍａｉｎｍｅｔ… 相似文献
18.
贺兰山北段早前寒武纪孔兹岩系的变质变形演化及动力学 总被引：6，自引：1，他引：5
通过对贺兰山北段孔兹岩系宏观及微观构造和典型变质矿物的详细研究,识别出该区曾经历了两个阶段四幕变形作用和三个阶段六幕变质作用,并结合矿物温历的估算,建立了该区变质作用演化的顺时针p-T-t-D轨迹,其反映本区孔兹岩系形成于陆陆碰撞的造山环境中,构造增厚作用是其发生的诱因。 相似文献
19.
Jiang Jisheng 《吉林大学学报(地球科学版)》1990,(2)
作为地壳早期演化阶段的一套变质沉积建造,孔兹岩系在原岩、成矿作用方面具其独有的特征和专属性。世界各地孔兹岩系的研究资料表明,其多数形成于太古代末及早元古初期,并经历了复杂的变质变形作用。同时含丰富的晶质石墨、富铝矿物、磷等非金属矿产,故孔兹岩系的系统研究对开发利用其矿产资源及推断地壳早期历史的演化,具有重大意义。本文对孔兹岩系原岩建造、变质作用、成矿作用及形成时代的研究现状作了概括介绍和评述。 相似文献
20.
This paper reports sensitive high resolution ion micro-probe U-Pb zircon ages for the "Huoqiu Group" and granitoids of the Early Precambrian basement in the Huoqiu area, southeastern margin of the North China Craton. The "Huoqiu Group" is similar in rock association and metamorphism to the khondalite series, apart from it containing considerable amounts of banded iron formation. All detrital zircons from the "Huoqiu Group" meta-sedimentary rocks are 3.0 Ga and 2.75 Ga, without any 2.5 Ga and younger ones, as is commonly found in Paleoproterozoic khondalite series in other areas of the North China Craton. In the Huoqiu area, 2.75 Ga and 2.56 Ga granitoids have also been identified. This basement assemblage underwent strong metamorphism during the late Paleoproterozoic (~1.84 Ga) tectonothermal event that is widely developed in the North China Craton. Thus the formation time of the "Huoqiu Group" can be constrained between 2.75 and 1.84 Ga in terms of detrital and metamorphic zircon ages. It is considered, combined with regional data, that there may be a Paleoproterozoic collision orogen extending in a NWW–SEE direction to the southern margin of the North China Craton. 相似文献