滨岸-浅海混合沉积对海平面与气候变化的响应&mdash;&mdash;以塔里木盆地巴麦地区石炭系为例

伏美燕; 李娜; 黄茜; 刘磊

doi:10.14027/j.cnki.cjxb.2017.06.003

ISSN 1000-0550 CN 62-1038/P

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滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例

伏美燕, 李娜, 黄茜, 刘磊

文章导航 > 沉积学报 > 2017 > 35(6): 1110-1120

伏美燕, 李娜, 黄茜, 刘磊. 滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例[J]. 沉积学报, 2017, 35(6): 1110-1120. doi: 10.14027/j.cnki.cjxb.2017.06.003

引用本文:

FU MeiYan, LI Na, HUANG Qian, LIU Lei. Shoreline-neritic Mixed Sedimentation Response to Sea Level Change and Paleoclimate: A case study from Carboniferous in Tarim Basin[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1110-1120. doi: 10.14027/j.cnki.cjxb.2017.06.003

Citation:

FU MeiYan, LI Na, HUANG Qian, LIU Lei. Shoreline-neritic Mixed Sedimentation Response to Sea Level Change and Paleoclimate: A case study from Carboniferous in Tarim Basin[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1110-1120. doi: 10.14027/j.cnki.cjxb.2017.06.003

引用本文:

Citation:

滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例

doi: 10.14027/j.cnki.cjxb.2017.06.003

伏美燕^1,2,3,
李娜^1,2,
黄茜¹,
刘磊¹

1.
成都理工大学能源学院, 成都 610059;
2.
油气藏地质及开发工程国家重点实验室(成都理工大学), 成都 610059;
3.
杜伦大学地球科学系, 英国杜伦 DH1 3LE

基金项目: 国家自然科学基金项目（41402096）

详细信息

作者简介:
伏美燕,女,1982年出生,博士,副教授,油气储层评价与油藏地球化学,E-mail:fumeiyan08@cdut.cn

中图分类号: P512.2;P595

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文章访问数: 443
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Shoreline-neritic Mixed Sedimentation Response to Sea Level Change and Paleoclimate: A case study from Carboniferous in Tarim Basin

FU MeiYan^1,2,3,
LI Na^1,2,
HUANG Qian¹,
LIU Lei¹

1.
College of Energy Resources, Chengdu University of Technology, Chengdu 610059, China;
2.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059, China;
3.
Department of Earth Science, Durham University, Durham DH1 3LE, UK

Funds: National Natural Science Foundation of China, No. 41402096

摘要

摘要: 陆源碎屑-碳酸盐混积作用发生的环境特征尚不明确，导致对混积岩分布规律认识不足。以塔里木盆地巴麦地区石炭系为例，通过薄片观察、矿物组成分析、主微量元素分析，对沉积环境和古环境特征参数进行了研究。研究区混积岩发育在障壁滨岸、碳酸盐岩局限台地和开阔台地。利用与混积强度相关性极好的Ti、Rb、K和Al的含量，将混积岩定量划分为4级。利用Na/Ca比值、Na含量分析了古盐度特征，Mn/Fe比值和Sr含量分析了古水深，用V/（V+Ni）比值反映了氧化还原条件，并利用Ti/Al，Mg/Sr反映了古气候特征。研究结果表明Ⅱ级以上混积均发生在湿润气候下，而干旱气候无明显混积，并且混合沉积大部分发生在海平面下降阶段。碳酸盐岩开阔台地的混积强度仅达I级，障壁滨岸和碳酸盐岩局限台地的混积强度较高，发育Ⅲ级和IV级高度混积岩。不同沉积环境的混合沉积均对古气候变化与相对海平面变化具有良好的响应，是详细的古环境变化记录。
- 塔里木盆地 /
- 混合沉积 /
- 古环境 /
- 古气候 /
- 海平面变化
Abstract: The characteristics of siliciclastic-carbonate mixed sedimentary environment still remains unknown, resulting in poor understanding of distribution of mixed rock. In this study, the sedimentary environments and environmental parameters of Carboniferous in Bamai area, Tarim Basin are deeply studied, using observation of thin sections, measurement of minerals composition, and elements composition. The mixed rocks were deposited, carbonate restricted platform and open platform. The concentrations of Ti, Rb, K, Al are used to divide the degrees of mixed sedimentation into four levels due to their good relationship with the degree of mixing. The salinity was reflected by Na content and Na/Ca. The depth of water was reflected by Mn/Fe and Sr content. The redox condition was reflected by V/(V+Ni). And, the paleoclimate was analyzed from Ti/Al and Mg/Sr. The result of geochemical indices shows the mixed sedimentation beyond Ⅱ level occurred at humid climate, while there was no obvious mixing at arid climate. Meanwhile, most mixed sedimentation accompanied by sea level fall. On the open platform, there was only I level mixed sedimentation, while Ⅲ-IV level mixed sedimentation developed on the barrier coast and restricted platform. The mixed sedimentation in each depositional environment can record the change of sea level and paleoclimate.
- Tarim Basin /
- mixed sedimentation /
- paleo-environment /
- paleoclimate /
- sea level change

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[1]	路淑毅, 杨斌, 李胜荣, 宋香锁, 杜圣贤, 高建飞, 张尚坤, 李明慧, 张伟林. 鲁西南单县盆地钻孔记录的古近纪环境变化 . 沉积学报, 2023, 41(2): 498-510. doi: 10.14027/j.issn.1000-0550.2021.090
[2]	张威, 马瑞丰, 刘亮, 杨蝉玉, 刘畅, 柴乐. 辽东半岛全新世沉积物记录的古气候变化研究进展 . 沉积学报, 2022, 40(5): 1355-1366. doi: 10.14027/j.issn.1000-0550.2021.009
[3]	高远, CarrollAlan R., 王成善. 异整合面——古环境剧变的地层记录 . 沉积学报, 2021, 39(1): 46-57. doi: 10.14027/j.issn.1000-0550.2020.128
[4]	郑伟, 刘云龙, 齐永安, 邢智峰, 李妲, 付玉鑫, 李婉颖, 许欣. 豫西荥阳P⁃Tr之交孙家沟组沉积环境及古气候变化 . 沉积学报, 2021, 39(5): 1128-1143. doi: 10.14027/j.issn.1000-0550.2020.059
[5]	陈留勤, 李鹏程, 郭福生, 刘鑫, 李馨敏. 粤北丹霞盆地晚白垩世丹霞组沉积相及古气候意义 . 沉积学报, 2019, 37(1): 17-29. doi: 10.14027/j.issn.1000-0550.2018.118
[6]	常吟善, 赵洪, 覃军, 李帅, 张建培. 古近纪气候变化在东海盆地内的化石记录 . 沉积学报, 2019, 37(2): 320-329. doi: 10.14027/j.issn.1000-0550.2018.133
[7]	陈留勤, 刘鑫, 李鹏程. 古土壤:沉积环境和古气候变化的灵敏指针 . 沉积学报, 2018, 36(3): 510-520. doi: 10.14027/j.issn.1000-0550.2018.054
[8]	王尹, 李祥辉, 周勇, 刘玲. 南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示 . 沉积学报, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
[9]	. 全新世以来巴里坤湖面积变化及气候环境记录 . 沉积学报, 2014, 32(1): 93-100.
[10]	. 柴达木盆地北缘下干柴沟组下段湖相混合沉积发育特征及其对储层的影响 . 沉积学报, 2013, 31(04): 724-729.
[11]	曹桐生. 内蒙古阿尔山地区下寒武统苏中组混合沉积特征及形成环境研究 . 沉积学报, 2011, 29(1): 55-63.
[12]	张西营. 德令哈盆地尕海湖DG03孔岩芯矿物组合与古环境变化 . 沉积学报, 2007, 25(5): 767-773.
[13]	唐永忠. 南秦岭古生代沉积盆地构造活动—海平面变化与沉积响应 . 沉积学报, 2007, 25(5): 653-662.
[14]	薛莲花, 陈国俊, 王琪, 史基安, 肖立新, 杨军, 赵克斌. 塔里木盆地K₂-E旋回层序与海平面变化 . 沉积学报, 1998, 16(3): 66-71.
[15]	杜小弟, 王璞君, 匡立春, 王东坡. 塔里木盆地震旦—泥盆纪古海平面变化再造及形成机理分析 . 沉积学报, 1997, 15(3): 14-17.
[16]	于炳松. 塔里木盆地北部寒武纪海平面变化研究 . 沉积学报, 1996, 14(1): 33-39.
[17]	江茂生, 沙庆安, 刘敏. 华北地台下中寒武统碳酸盐与陆源碎屑混合沉积──以山东张夏地区为例 . 沉积学报, 1996, 14(S1): 63-74.
[18]	吉利明. 甘肃民和盆地早白垩世孢粉植物群的古气候环境和地理分区位置 . 沉积学报, 1994, 12(2): 133-142.
[19]	范善发, 周中毅, 潘长春. 应用生物标志物评价塔里木盆地下古生界沉积物的古环境 . 沉积学报, 1991, 9(S1): 44-51.
[20]	费富安. 对苏北含油盆地下第三系古环境和古气候的探讨 . 沉积学报, 1988, 6(1): 21-28.

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滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例

doi: 10.14027/j.cnki.cjxb.2017.06.003

1. 成都理工大学能源学院, 成都 610059;

2. 油气藏地质及开发工程国家重点实验室(成都理工大学), 成都 610059;

3. 杜伦大学地球科学系, 英国杜伦 DH1 3LE

基金项目: 国家自然科学基金项目（41402096）

作者简介:
伏美燕,女,1982年出生,博士,副教授,油气储层评价与油藏地球化学,E-mail:fumeiyan08@cdut.cn

收稿日期: 2017-04-20
修回日期: 2017-05-29
刊出日期: 2017-12-10

中图分类号: P512.2;P595

关键词:

塔里木盆地 /

混合沉积 /

古环境 /

古气候 /

海平面变化

摘要: 陆源碎屑-碳酸盐混积作用发生的环境特征尚不明确，导致对混积岩分布规律认识不足。以塔里木盆地巴麦地区石炭系为例，通过薄片观察、矿物组成分析、主微量元素分析，对沉积环境和古环境特征参数进行了研究。研究区混积岩发育在障壁滨岸、碳酸盐岩局限台地和开阔台地。利用与混积强度相关性极好的Ti、Rb、K和Al的含量，将混积岩定量划分为4级。利用Na/Ca比值、Na含量分析了古盐度特征，Mn/Fe比值和Sr含量分析了古水深，用V/（V+Ni）比值反映了氧化还原条件，并利用Ti/Al，Mg/Sr反映了古气候特征。研究结果表明Ⅱ级以上混积均发生在湿润气候下，而干旱气候无明显混积，并且混合沉积大部分发生在海平面下降阶段。碳酸盐岩开阔台地的混积强度仅达I级，障壁滨岸和碳酸盐岩局限台地的混积强度较高，发育Ⅲ级和IV级高度混积岩。不同沉积环境的混合沉积均对古气候变化与相对海平面变化具有良好的响应，是详细的古环境变化记录。

English Abstract

Shoreline-neritic Mixed Sedimentation Response to Sea Level Change and Paleoclimate: A case study from Carboniferous in Tarim Basin

1. College of Energy Resources, Chengdu University of Technology, Chengdu 610059, China;

2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059, China;

3. Department of Earth Science, Durham University, Durham DH1 3LE, UK

Funds: National Natural Science Foundation of China, No. 41402096

Received Date: 2017-04-20
Rev Recd Date: 2017-05-29
Publish Date: 2017-12-10

Keywords:

Abstract: The characteristics of siliciclastic-carbonate mixed sedimentary environment still remains unknown, resulting in poor understanding of distribution of mixed rock. In this study, the sedimentary environments and environmental parameters of Carboniferous in Bamai area, Tarim Basin are deeply studied, using observation of thin sections, measurement of minerals composition, and elements composition. The mixed rocks were deposited, carbonate restricted platform and open platform. The concentrations of Ti, Rb, K, Al are used to divide the degrees of mixed sedimentation into four levels due to their good relationship with the degree of mixing. The salinity was reflected by Na content and Na/Ca. The depth of water was reflected by Mn/Fe and Sr content. The redox condition was reflected by V/(V+Ni). And, the paleoclimate was analyzed from Ti/Al and Mg/Sr. The result of geochemical indices shows the mixed sedimentation beyond Ⅱ level occurred at humid climate, while there was no obvious mixing at arid climate. Meanwhile, most mixed sedimentation accompanied by sea level fall. On the open platform, there was only I level mixed sedimentation, while Ⅲ-IV level mixed sedimentation developed on the barrier coast and restricted platform. The mixed sedimentation in each depositional environment can record the change of sea level and paleoclimate.

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滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例

doi: 10.14027/j.cnki.cjxb.2017.06.003

作者简介:
伏美燕,女,1982年出生,博士,副教授,油气储层评价与油藏地球化学,E-mail:fumeiyan08@cdut.cn

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Shoreline-neritic Mixed Sedimentation Response to Sea Level Change and Paleoclimate: A case study from Carboniferous in Tarim Basin

计量

目录

滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例

doi: 10.14027/j.cnki.cjxb.2017.06.003

1. 成都理工大学能源学院, 成都 610059;

2. 油气藏地质及开发工程国家重点实验室(成都理工大学), 成都 610059;

3. 杜伦大学地球科学系, 英国杜伦 DH1 3LE

作者简介:
伏美燕,女,1982年出生,博士,副教授,油气储层评价与油藏地球化学,E-mail:fumeiyan08@cdut.cn

English Abstract

Shoreline-neritic Mixed Sedimentation Response to Sea Level Change and Paleoclimate: A case study from Carboniferous in Tarim Basin

1. College of Energy Resources, Chengdu University of Technology, Chengdu 610059, China;

2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059, China;

3. Department of Earth Science, Durham University, Durham DH1 3LE, UK

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滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例

doi: 10.14027/j.cnki.cjxb.2017.06.003

作者简介: 伏美燕,女,1982年出生,博士,副教授,油气储层评价与油藏地球化学,E-mail:fumeiyan08@cdut.cn

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Shoreline-neritic Mixed Sedimentation Response to Sea Level Change and Paleoclimate: A case study from Carboniferous in Tarim Basin

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出版历程

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滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例

doi: 10.14027/j.cnki.cjxb.2017.06.003

1. 成都理工大学能源学院, 成都 610059; 2. 油气藏地质及开发工程国家重点实验室(成都理工大学), 成都 610059; 3. 杜伦大学地球科学系, 英国杜伦 DH1 3LE

作者简介: 伏美燕,女,1982年出生,博士,副教授,油气储层评价与油藏地球化学,E-mail:fumeiyan08@cdut.cn

English Abstract

Shoreline-neritic Mixed Sedimentation Response to Sea Level Change and Paleoclimate: A case study from Carboniferous in Tarim Basin

1. College of Energy Resources, Chengdu University of Technology, Chengdu 610059, China; 2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059, China; 3. Department of Earth Science, Durham University, Durham DH1 3LE, UK

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目录

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期刊在线

联系我们

作者简介:
伏美燕,女,1982年出生,博士,副教授,油气储层评价与油藏地球化学,E-mail:fumeiyan08@cdut.cn

1. 成都理工大学能源学院, 成都 610059;

2. 油气藏地质及开发工程国家重点实验室(成都理工大学), 成都 610059;

3. 杜伦大学地球科学系, 英国杜伦 DH1 3LE

作者简介:
伏美燕,女,1982年出生,博士,副教授,油气储层评价与油藏地球化学,E-mail:fumeiyan08@cdut.cn

1. College of Energy Resources, Chengdu University of Technology, Chengdu 610059, China;

2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059, China;

3. Department of Earth Science, Durham University, Durham DH1 3LE, UK