碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示

李双建

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示

李双建

文章导航 > 沉积学报 > 2006 > 24(1): 28-35

李双建. 碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示[J]. 沉积学报, 2006, 24(1): 28-35.

引用本文:

李双建. 碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示[J]. 沉积学报, 2006, 24(1): 28-35.

LI Shuangjian. The Analysis of Detrital Heavy Minerals in CretaceousTertiary Sandstones, Kuqa Depression and Their Implications for Provenance [J]. Acta Sedimentologica Sinica, 2006, 24(1): 28-35.

Citation:

LI Shuangjian. The Analysis of Detrital Heavy Minerals in CretaceousTertiary Sandstones, Kuqa Depression and Their Implications for Provenance [J]. Acta Sedimentologica Sinica, 2006, 24(1): 28-35.

李双建. 碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示[J]. 沉积学报, 2006, 24(1): 28-35.

引用本文:

李双建. 碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示[J]. 沉积学报, 2006, 24(1): 28-35.

Citation:

碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示

李双建

中国科学院地质与地球物理研究所北京 100029

详细信息

通讯作者:
李双建

计量

文章访问数: 1876
HTML全文浏览量: 32
PDF下载量: 794
被引次数: 0

The Analysis of Detrital Heavy Minerals in CretaceousTertiary Sandstones, Kuqa Depression and Their Implications for Provenance 

LI Shuangjian

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

More Information

Corresponding author: LI Shuangjian

摘要

摘要: 碎屑沉积是山脉隆升和盆地沉积的直接记录，包括碎屑重矿物研究在内的碎屑沉积物的分析是开展盆山耦合研究的必要手段。对库车坳陷白垩系—第三系砂岩中重矿物含量特征进行了系统的研究，并应用电子探针技术分析碎屑石榴石和钛铁矿的化学组成，研究表明库车坳陷白垩—第三系源区主要由沉积岩、变质岩和酸性火山岩组成。白垩系砂岩中的石榴石来自西南天山蓝片岩和低级变质岩的比例较大，而第三系砂岩中的石榴石中富铁铝榴石组分，多来自高级变质岩。白垩系砂岩中的钛铁矿多来自变质岩，上第三系砂岩中来自火成岩的钛铁矿比例增加。由此可以认为南天山的大规模隆升和剥蚀发生在第三纪以来，由于它的隆升遮挡了南天山北缘古生代增生杂岩体对库车坳陷的物质贡献，并且随着剥蚀的加深，高级变质岩和火成岩的出露越来越多。
- 重矿物 /
- 库车坳陷 /
- 南天山 /
- 物源 /
- 电子探针 /
- 石榴石 /
- 钛铁矿
Abstract: Detrital sedimentation is the direct record in basin for mountain uplift and erosion. The analysis of detrital minerals, including heavy minerals, is a key means for basinmountain coupling studies. The distribution characteristics of heavy minerals in CretaceousTertiary sandstones, Kuqa depression have been studied systemically in this paper, and chemical compositions of detrital garnets and ilmenites have been analyzed by electronic microprobe. The results illustrate that the provenance area of CretaceousTertiary〖KG*2〗sandstones, Kuqa depression, are mainly composed of sedimentary rocks, metamorphic rocks and little intermediatefelsic igneous rocks.〖KG*2〗The〖KG*2〗garnets in Cretaceous sandstones come from blueschist that〖KG*2〗located in the southwest〖KG*2〗Tianshan and lowgrade metamorphic rocks by lager proportionally. The garnets in Tertiary sandstones enrich almandine, which come from highgrade metamorphic rocks. The provenance of most ilmenites in Cretaceous sandstones is metamorphic rocks, and the proportion of igneous rocks provenance increase in Tertiary. These analysis show that southern Tianshan uplift and erosion extensively from Tertiary, as a result of which the provenance of blue schist〖KG*2〗in Paleozoic accretion from north margin of south〖KG*2〗Tianshan has been curtained. With〖KG*2〗deeply erosion of Tianshan, more and more highgrade metamorphic and igneous rocks are exposed.
- heavy mineral /
- Kuqa depression /
- southern Tianshan /
- provenance /
- electronic microprobe /
- garnet /
- ilmenite

HTML全文

参考文献(0)

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 1876
HTML全文浏览量: 32
PDF下载量: 794
被引次数: 0

碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示

李双建

中国科学院地质与地球物理研究所北京 100029

通讯作者: 李双建

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2006-02-10

关键词:

重矿物 /

库车坳陷 /

南天山 /

物源 /

电子探针 /

石榴石 /

钛铁矿

摘要: 碎屑沉积是山脉隆升和盆地沉积的直接记录，包括碎屑重矿物研究在内的碎屑沉积物的分析是开展盆山耦合研究的必要手段。对库车坳陷白垩系—第三系砂岩中重矿物含量特征进行了系统的研究，并应用电子探针技术分析碎屑石榴石和钛铁矿的化学组成，研究表明库车坳陷白垩—第三系源区主要由沉积岩、变质岩和酸性火山岩组成。白垩系砂岩中的石榴石来自西南天山蓝片岩和低级变质岩的比例较大，而第三系砂岩中的石榴石中富铁铝榴石组分，多来自高级变质岩。白垩系砂岩中的钛铁矿多来自变质岩，上第三系砂岩中来自火成岩的钛铁矿比例增加。由此可以认为南天山的大规模隆升和剥蚀发生在第三纪以来，由于它的隆升遮挡了南天山北缘古生代增生杂岩体对库车坳陷的物质贡献，并且随着剥蚀的加深，高级变质岩和火成岩的出露越来越多。

English Abstract

The Analysis of Detrital Heavy Minerals in CretaceousTertiary Sandstones, Kuqa Depression and Their Implications for Provenance 

LI Shuangjian

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

Corresponding author: LI Shuangjian

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2006-02-10

Keywords:

Abstract: Detrital sedimentation is the direct record in basin for mountain uplift and erosion. The analysis of detrital minerals, including heavy minerals, is a key means for basinmountain coupling studies. The distribution characteristics of heavy minerals in CretaceousTertiary sandstones, Kuqa depression have been studied systemically in this paper, and chemical compositions of detrital garnets and ilmenites have been analyzed by electronic microprobe. The results illustrate that the provenance area of CretaceousTertiary〖KG*2〗sandstones, Kuqa depression, are mainly composed of sedimentary rocks, metamorphic rocks and little intermediatefelsic igneous rocks.〖KG*2〗The〖KG*2〗garnets in Cretaceous sandstones come from blueschist that〖KG*2〗located in the southwest〖KG*2〗Tianshan and lowgrade metamorphic rocks by lager proportionally. The garnets in Tertiary sandstones enrich almandine, which come from highgrade metamorphic rocks. The provenance of most ilmenites in Cretaceous sandstones is metamorphic rocks, and the proportion of igneous rocks provenance increase in Tertiary. These analysis show that southern Tianshan uplift and erosion extensively from Tertiary, as a result of which the provenance of blue schist〖KG*2〗in Paleozoic accretion from north margin of south〖KG*2〗Tianshan has been curtained. With〖KG*2〗deeply erosion of Tianshan, more and more highgrade metamorphic and igneous rocks are exposed.

李双建. 碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示[J]. 沉积学报, 2006, 24(1): 28-35.

引用本文:

李双建. 碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示[J]. 沉积学报, 2006, 24(1): 28-35.

Citation:

全文HTML

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

[1]	苏展艺, 姚付龙, 夏倩倩, 胡晓峰. 中天山山间盆地中晚全新世植被与气候变化 . 沉积学报, 2026, 44(2): 415-424. doi: 10.14027/j.issn.1000-0550.2024.058
[2]	胡涛, 庞雄奇, 姜福杰, 王琦峰, 徐田武, 吴冠昀, 蔡哲, 于吉旺. 陆相断陷咸化湖盆有机质差异富集因素探讨 . 沉积学报, 2021, 39(1): 140-152. doi: 10.14027/j.issn.1000-0550.2020.125
[3]	段知非, 李超, 毕磊, 何中发, 李芳亮, 杨守业. 崇明岛H12孔百年来长江入海沉积物来源变化及原因 . 沉积学报, 2020, 38(6): 1204-1214. doi: 10.14027/j.issn.1000-0550.2020.002
[4]	张平. 稳定湖相沉积物和风成黄土粒度判别函数的建立及其意义 . 沉积学报, 2008, 26(3): 501-507.
[5]	陈陵康郭建秋顾延生. 西藏拉萨河现代河漫滩及一级阶地沉积物植硅体组合特征 . 沉积学报, 2008, 26(3): 480-486.
[6]	郭彦如刘化清李相博完颜容郑希民. 大型坳陷湖盆层序地层格架的研究方法体系 ———以鄂尔多斯盆地中生界延长组为例 . 沉积学报, 2008, 26(3): 384-391.

留言板

碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示

通讯作者:
李双建

计量

The Analysis of Detrital Heavy Minerals in CretaceousTertiary Sandstones, Kuqa Depression and Their Implications for Provenance 

Corresponding author: LI Shuangjian

计量

目录

碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示

中国科学院地质与地球物理研究所北京 100029

通讯作者: 李双建

English Abstract

The Analysis of Detrital Heavy Minerals in CretaceousTertiary Sandstones, Kuqa Depression and Their Implications for Provenance 

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

Corresponding author: LI Shuangjian

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示

通讯作者: 李双建

计量

出版历程

The Analysis of Detrital Heavy Minerals in CretaceousTertiary Sandstones, Kuqa Depression and Their Implications for Provenance 

Corresponding author: LI Shuangjian

计量

出版历程

目录

碎屑重矿物分析对库车坳陷白垩—第三纪物源变化的指示

中国科学院地质与地球物理研究所 北京 100029

通讯作者: 李双建

English Abstract

The Analysis of Detrital Heavy Minerals in CretaceousTertiary Sandstones, Kuqa Depression and Their Implications for Provenance 

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

Corresponding author: LI Shuangjian

全文HTML

目录

友情链接

期刊在线

联系我们

通讯作者:
李双建

中国科学院地质与地球物理研究所北京 100029