新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境

王东安; 陈瑞君

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

新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境

王东安, 陈瑞君

文章导航 > 沉积学报 > 1995 > 13(3): 13-22

王东安, 陈瑞君. 新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境[J]. 沉积学报, 1995, 13(3): 13-22.

引用本文:

王东安, 陈瑞君. 新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境[J]. 沉积学报, 1995, 13(3): 13-22.

Wang Dongan, Chen Ruijun. The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang[J]. Acta Sedimentologica Sinica, 1995, 13(3): 13-22.

Citation:

Wang Dongan, Chen Ruijun. The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang[J]. Acta Sedimentologica Sinica, 1995, 13(3): 13-22.

王东安, 陈瑞君. 新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境[J]. 沉积学报, 1995, 13(3): 13-22.

引用本文:

王东安, 陈瑞君. 新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境[J]. 沉积学报, 1995, 13(3): 13-22.

Wang Dongan, Chen Ruijun. The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang[J]. Acta Sedimentologica Sinica, 1995, 13(3): 13-22.

Citation:

Wang Dongan, Chen Ruijun. The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang[J]. Acta Sedimentologica Sinica, 1995, 13(3): 13-22.

新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境

中国科学院地质研究所北京 100029

基金项目: 中国科学院国家自然科学基金

详细信息

作者简介:
王东安,,男,57岁,副研究员,沉积学

计量

文章访问数: 533
HTML全文浏览量: 1
PDF下载量: 415
被引次数: 0

The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang

Institute of Geology, Chinese Academy of Science, Beijing 100029

摘要

摘要: 在西昆仑北带沉积区中，泥盆系沉积是该区古生代最早的沉积层，它超覆在中上元古代沉积层之上。在莫木克以南克兹扬鲁克一带，泥盆纪中上段地层发育较好，颇有代表性。这套沉积层根据岩石组合分为上下两段，下段是一套富含凝灰质的碎屑岩一碳酸盐岩建造。具有重力流的沉积特点。上段是一套陆屑砂砾岩－杂砂岩建造，属于滨海海滩相、滨海近岸三角洲相、河流相沉积。
- 西昆仑 /
- 泥盆系 /
- 沉积岩特征 /
- 沉积环境 /
- 克兹扬鲁克
Abstract: The Devonian strain are developed on the north margin of the West Kunlun Mt. They are the oldest Paleozoic sedimentary rocks in this region and overlapped on the Middle-Upper Proterozoic strata. To the south of Monk, the Middle-Upper Devonian is well developed in the Keziyangluk area.According to the lithological features and rock associations, they can be divided into two members. The lower one is a tuffaceous graywacke carbonate rock formation, composed of tuffaceous graywacke, tuffaceous shale, pebble-bearing sandy slate and carbonate rock. The upper member is a terrigenous sandy conglomerate graywacke formation, composed of conglomerate,sandy conglomerate, lithic graywacke,quartzose graywacke, silstone, etc. The lower member is characterized by laminar bedding and horizontal bedding, indicating a steady hydrodynamic sedimentary environment. The upper member comprises torrigenous sand and Pebble sediments with clear cyclicity. Its different horizons show different sedimentary structures, such as horizontal bedding, various cross-bedding and interference ripple, indicating an unstable sedimentary water body and unsteady sedimentary factes.The studies on sedimentary structures and lithological grain features of the Middle Upper Devonian strata suggest that the lower member is formed in a bathyal-neritic sedimentary environment. and that the upper member is developed in an littoral beach inshore deltufluvial sedimentary environment.
- West Kunlun /
- Devonian /
- Sedimentary rock features /
- Sedimentary /
- environment Keziyangluk

HTML全文

参考文献(1)

[1]

1.尹集祥，徐均涛，刘成杰等，1990，拉萨至格尔木的区域地层，青藏高原地质演化，北京:科学出版社，1-46。

2.刘训，傅德荣，姚培毅等，1992，青藏高原不同地体的地层，生物区系及沉积构造演化历史，北京:地质出版社，68-73。

3.孙东立.罗辉，1990，昆仑山阿其克库勒湖地区泥盆系研究的新进展，地层学杂志，14(3);43-46。

4.陈瑞君，车春兰，1986，苏北盆地下第三系碎屑岩的粒度分布特征及其环境解释，岩石学报，2(4):73 -82。

5.徐宪，魏永声，陈国恩等，1982，青茂藏高原区域地层简表，北京:地质出版社，1 -163。

6.潘裕生主编，1992，喀喇昆仑山一昆仑山综合科学考察导论，北京:气象出版社，1-8。

7.Folk, R. L.，1966. A review of grain一size parameters. secimentology. 6 (1),73-93.

8.Sahu, B. K.，1964，Significance of the size-distribution statistics in the interpretation of depasitional environments. Res.Bull.，N. S.，Punmb univ. 15(1);213一219.

9.Vishet.9. G. S.，1969. Grain size destributions and depasitional processes. J. Sediment. Petrol. 39(5):1074一1106.

[1]	张莹, 陈少平, 刘志峰, 杨东升, 耿名扬, 吴斌. 沉积环境对渤海金西A洼烃源岩的控制作用 . 沉积学报, 2023, 41(3): 890-900. doi: 10.14027/j.issn.1000-0550.2022.047
[2]	张治波, 徐颖, 苗艳菊, 王文锋, 赵迪斐, 陈丹玲. 昌都盆地古近系贡觉组物源及其沉积环境 . 沉积学报, 2022, 40(6): 1561-1581. doi: 10.14027/j.issn.1000-0550.2022.094
[3]	陈登辉, 隋清霖, 赵晓健, 荆德龙, 滕家欣, 高永宝. 西昆仑穆呼锰矿晚石炭世含锰碳酸盐岩地质地球化学特征及其沉积环境 . 沉积学报, 2019, 37(3): 477-490. doi: 10.14027/j.issn.1000-0550.2018.157
[4]	刘沛显, 关平, 冯帆, 贾文博, 张巍, 邓世彪, 金亦秋. 塔西台地寒武纪沉积环境演化与海陆耦合 . 沉积学报, 2016, 34(6): 1092-1107. doi: 10.14027/j.cnki.cjxb.2016.06.008
[5]	牛永斌, 单婷婷, 董小波, 周硕, 高文秀. 豫西北奥陶系马家沟组遗迹化石及其沉积环境 . 沉积学报, 2015, 33(2): 211-225. doi: 10.14027/j.cnki.cjxb.2015.02.001
[6]	时文革, 巩恩普, 褚亦功, 张永利, 姚玉增, 王铁晖, 马伟, 赵纯福. 新疆拜城新近系含铜岩系沉积体系及沉积环境 . 沉积学报, 2015, 33(6): 1074-1086. doi: 10.14027/j.cnki.cjxb.2015.06.002
[7]	张哲杜远生毛治超李瑞原小杰. 湘东南桂阳莲塘上泥盆系风暴岩特征及其古地理、古气候意义 . 沉积学报, 2008, 26(3): 369-375.
[8]	方维萱, 张国伟, 胡瑞忠, 刘方杰. 秦岭造山带泥盆系热水沉积岩相应用研究及实例 . 沉积学报, 2001, 19(1): 48-54.
[9]	徐天光, 顾家裕, 薛叔浩. 塔里木盆地轮台断隆第三系盐湖沉积环境研究 . 沉积学报, 1998, 16(3): 137-140.
[10]	邱艳生. 山西襄汾奥陶系岩石学特征及沉积环境分析 . 沉积学报, 1993, 11(4): 67-72.
[11]	宋春晖, 武安斌. 西成矿田中泥盆统碳酸盐岩沉积微相、微相组及其环境分析 . 沉积学报, 1993, 11(2): 34-42.
[12]	龚一鸣. 新疆北部泥盆系火山碎屑浊积岩层序结构特征及其地质意义 . 沉积学报, 1993, 11(2): 75-83.
[13]	许凤仪. 西成铅锌矿田西部中泥盆统西汉水组碳酸盐岩沉积特征 . 沉积学报, 1991, 9(1): 81-86.
[14]	朱莲芳, 马宝林. 塔里木盆地阿克苏—柯坪地区寒武系—奥陶系的沉积环境 . 沉积学报, 1991, 9(2): 55-62.
[15]	杜远生, 赵锡文. 甘肃西成铅锌矿田泥盆纪吉维特—弗拉斯期沉积古地理及控矿意义 . 沉积学报, 1991, 9(3): 22-30.
[16]	郑庆年. 再论凡口矿区中上泥盆统叠层石及其地层沉积环境意义 . 沉积学报, 1990, 8(3): 103-109.
[17]	刘文均. 湘南泥盆系碳酸盐岩中锶的分布特点及其环境意义 . 沉积学报, 1989, 7(2): 14-20.
[18]	高计元. 中国南方泥盆系瘤状灰岩的成因 . 沉积学报, 1988, 6(2): 77-86.
[19]	栾绍堃. 青海祁连含煤区侏罗纪含煤岩系沉积环境 . 沉积学报, 1987, 5(1): 132-136.
[20]	陈先沛, 高计元. 广西中部泥盆系的多金属-重晶石矿床和热水沉积作用 . 沉积学报, 1987, 5(3): 149-158.

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: 533
HTML全文浏览量: 1
PDF下载量: 415
被引次数: 0

新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境

中国科学院地质研究所北京 100029

基金项目: 中国科学院国家自然科学基金

作者简介:
王东安,,男,57岁,副研究员,沉积学

收稿日期: 1994-10-17
刊出日期: 1995-09-10

关键词:

西昆仑 /

泥盆系 /

沉积岩特征 /

沉积环境 /

克兹扬鲁克

摘要: 在西昆仑北带沉积区中，泥盆系沉积是该区古生代最早的沉积层，它超覆在中上元古代沉积层之上。在莫木克以南克兹扬鲁克一带，泥盆纪中上段地层发育较好，颇有代表性。这套沉积层根据岩石组合分为上下两段，下段是一套富含凝灰质的碎屑岩一碳酸盐岩建造。具有重力流的沉积特点。上段是一套陆屑砂砾岩－杂砂岩建造，属于滨海海滩相、滨海近岸三角洲相、河流相沉积。

English Abstract

The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang

Institute of Geology, Chinese Academy of Science, Beijing 100029

Received Date: 1994-10-17
Publish Date: 1995-09-10

Keywords:

Abstract: The Devonian strain are developed on the north margin of the West Kunlun Mt. They are the oldest Paleozoic sedimentary rocks in this region and overlapped on the Middle-Upper Proterozoic strata. To the south of Monk, the Middle-Upper Devonian is well developed in the Keziyangluk area.According to the lithological features and rock associations, they can be divided into two members. The lower one is a tuffaceous graywacke carbonate rock formation, composed of tuffaceous graywacke, tuffaceous shale, pebble-bearing sandy slate and carbonate rock. The upper member is a terrigenous sandy conglomerate graywacke formation, composed of conglomerate,sandy conglomerate, lithic graywacke,quartzose graywacke, silstone, etc. The lower member is characterized by laminar bedding and horizontal bedding, indicating a steady hydrodynamic sedimentary environment. The upper member comprises torrigenous sand and Pebble sediments with clear cyclicity. Its different horizons show different sedimentary structures, such as horizontal bedding, various cross-bedding and interference ripple, indicating an unstable sedimentary water body and unsteady sedimentary factes.The studies on sedimentary structures and lithological grain features of the Middle Upper Devonian strata suggest that the lower member is formed in a bathyal-neritic sedimentary environment. and that the upper member is developed in an littoral beach inshore deltufluvial sedimentary environment.

王东安, 陈瑞君. 新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境[J]. 沉积学报, 1995, 13(3): 13-22.

引用本文:

王东安, 陈瑞君. 新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境[J]. 沉积学报, 1995, 13(3): 13-22.

Wang Dongan, Chen Ruijun. The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang[J]. Acta Sedimentologica Sinica, 1995, 13(3): 13-22.

Citation:

Wang Dongan, Chen Ruijun. The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang[J]. Acta Sedimentologica Sinica, 1995, 13(3): 13-22.

全文HTML

参考文献 (1)

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

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境

作者简介:
王东安,,男,57岁,副研究员,沉积学

计量

The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang

计量

目录

新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境

中国科学院地质研究所北京 100029

作者简介:
王东安,,男,57岁,副研究员,沉积学

English Abstract

The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang

Institute of Geology, Chinese Academy of Science, Beijing 100029

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境

作者简介: 王东安,,男,57岁,副研究员,沉积学

计量

出版历程

The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang

计量

出版历程

目录

新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境

中国科学院地质研究所 北京 100029

作者简介: 王东安,,男,57岁,副研究员,沉积学

English Abstract

The Characteristics of Devonian Sedimentary Rocks and Their Sedimentary Environments in the Keziyangluk area, Xinjiang

Institute of Geology, Chinese Academy of Science, Beijing 100029

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
王东安,,男,57岁,副研究员,沉积学

中国科学院地质研究所北京 100029

作者简介:
王东安,,男,57岁,副研究员,沉积学