干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例

陈  波

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干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例

陈波

文章导航 > 沉积学报 > 2007 > 25(1): 21-28

陈波. 干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例[J]. 沉积学报, 2007, 25(1): 21-28.

引用本文:

陈波. 干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例[J]. 沉积学报, 2007, 25(1): 21-28.

CHEN Bo. Characteristics of Lacustrine Highresolution Sequence Stratigraphy underArid Climate : a case study of Yuyang Formation (Late Cretaceous) in Southwest of Jianghan Basin[J]. Acta Sedimentologica Sinica, 2007, 25(1): 21-28.

Citation:

陈波. 干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例[J]. 沉积学报, 2007, 25(1): 21-28.

引用本文:

陈波. 干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例[J]. 沉积学报, 2007, 25(1): 21-28.

Citation:

干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例

陈波

油气资源与勘探技术教育部重点实验室长江大学地球科学学院湖北荆州 434023

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通讯作者:
陈波

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Characteristics of Lacustrine Highresolution Sequence Stratigraphy underArid Climate : a case study of Yuyang Formation (Late Cretaceous) in Southwest of Jianghan Basin

CHEN Bo

Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education, Yangtze University Jingzhou, Hubei 434023

More Information

Corresponding author: CHEN Bo

摘要

摘要: 江汉盆地西南缘白垩系上统渔洋组地层旋回主要受气候因素的影响。研究区渔洋组是在干旱气候条件下沉积的洪水—漫湖沉积体系，其气候变化的特点是短暂洪水期与较长干旱的间洪水期交替变化，同时表现出不同级别的旋回，在气候越来越干旱的背景下，洪水期持续的时间就会越短，洪水的规模也越来越小。在短期的气候变化旋回下，地层沉积特征表现为洪水期沉积的水道、砂坪等微相与干旱的间洪水期泥坪微相互层。在中期气候变化旋回下，主洪水期持续时间长、规模大，沉积分布广泛,形成较厚的灰色水道砂岩沉积和灰色泥岩沉积夹薄层的红色泥坪沉积，间洪水期沉积为砂坪、混合坪与泥坪互层构成。长期旋回表现为每个中期主洪水期越来越小、水道沉积规模变小，间洪水期形成的红色泥坪厚度逐渐加厚，代表气候越来越干旱。研究区的这种地层旋回变化特征反映出气候是地层旋回的主控因素，不仅控制地层的短期旋回，同时控制地层的中长期旋回。这些特征具明显的等时性和可对比性，为油田开发过程中小层对比及油层划分提供了理论依据。
- 江陵凹陷 /
- 渔洋组 /
- 气候演变 /
- 洪水期 /
- 间洪水期 /
- 基准面变化
Abstract: The sequence in Yuyang Formation of lateCretaceous in southwest of Jianghan Basin is controlled by arid climate. Due to the evolution of climate, the flood period and interflood period alternately occur. In shortterm cycle, the sandstone of channel microfacies and sandflat microfacies deposits in flood period and the mudstone of mudflat microfacies deposits in interflood period. In midterm cycle, there appear several assemblages of shortterm sequence cycle. The main flood period usually lasts quite a long time with a large scale, so there deposits a set of thick grey sandstone of channel microfacies and mudstone of distal microfacies with interlayers of laminar red mudstone of mudflat microfacies .Moreover, there is a set of sandflat, mixedflat and mudflat microfacies in the main interflood period. Different from the two cycles above, in longterm cycle, it has a trend that the scales of the channel decrease in main flood period while the thicknesses of red mudflat increase in interflood period. All these characters in mid& longterm sequence cycle suggest the climate has a tendency to become more and more arid. In terms of the characters of sequences and microfacies in arid climate evolution, the authors build up a set of highresolution stratigraphic sequence and make the stratigraphic correlation.
- Jianghan Basin /
- Yuyang Formation /
- highresolution sequence stratigraphy /
- flood period & /
- interflood period /
- baselevel cycle

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[1]	张力钰, 陈代钊, 刘康. 弗拉—法门转折期气候—海洋环境变化及生物危机成因探讨 . 沉积学报, 2024, 42(3): 723-737. doi: 10.14027/j.issn.1000-0550.2023.107
[2]	李梦茹, 唐友军, 杨易卓, 于瑾. 江陵凹陷古近系新沟嘴组下段原油芳烃馏分地球化学特征及油源对比 . 沉积学报, 2024, 42(1): 266-281. doi: 10.14027/j.issn.1000-0550.2022.026
[3]	陈公哲, 陈仕涛, 刘笑, 赵侃, 王真军, 张振球, 汪永进. 倒数第三次冰消期气候变化的石笋多指标分析 . 沉积学报, 2023, 41(4): 992-1001. doi: 10.14027/j.issn.1000-0550.2022.020
[4]	梁晓伟, 鲜本忠, 冯胜斌, 陈鹏, 尤源, 吴千然, 淡卫东, 张文淼. 鄂尔多斯盆地陇东地区长7段重力流砂体构型及其主控因素 . 沉积学报, 2022, 40(3): 641-652. doi: 10.14027/j.issn.1000-0550.2021.017
[5]	李跃, 李军辉, 王子赫, 李美芳, 娄洪, 王琦, 孙海雷. 陆相断陷湖盆基准面旋回对沉积砂体的控制——以海拉尔盆地贝尔凹陷贝西地区为例 . 沉积学报, 2019, 37(4): 858-867. doi: 10.14027/j.issn.1000-0550.2018.179
[6]	陈亮, 季汉成, 张靓, 李晨, 时聪, 于斌. 裂陷盆地重力流沉积对基准面变化的响应——以乌里雅斯太南洼腾一下亚段为例 . 沉积学报, 2016, 34(3): 487-496. doi: 10.14027/j.cnki.cjxb.2016.03.006
[7]	杨延强, 吴胜和, 岳大力, 兰献娇, 李艳杰, 沈云奇. 长期基准面旋回内河口坝构型的演化规律——以胜坨油田坨7断块沙二段下油组为例 . 沉积学报, 2015, 33(2): 326-336. doi: 10.14027/j.cnki.cjxb.2015.02.012
[8]	陈贤良, 纪友亮, 杨克明, 刘君龙, 黄富祥, 赵春妮, 杨永, 李龙迪. 川西坳陷上侏罗统遂宁组洪水—漫湖沉积特征 . 沉积学报, 2014, 32(5): 912-920.
[9]	崔景伟. 冀北凹陷高于庄组与洪水庄组在岩芯、露头中多赋存态生物标志物的对比 . 沉积学报, 2011, 29(3): 593-598.
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干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例

陈波

油气资源与勘探技术教育部重点实验室长江大学地球科学学院湖北荆州 434023

通讯作者: 陈波

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2007-02-10

关键词:

渔洋组 /

洪水期 /

摘要: 江汉盆地西南缘白垩系上统渔洋组地层旋回主要受气候因素的影响。研究区渔洋组是在干旱气候条件下沉积的洪水—漫湖沉积体系，其气候变化的特点是短暂洪水期与较长干旱的间洪水期交替变化，同时表现出不同级别的旋回，在气候越来越干旱的背景下，洪水期持续的时间就会越短，洪水的规模也越来越小。在短期的气候变化旋回下，地层沉积特征表现为洪水期沉积的水道、砂坪等微相与干旱的间洪水期泥坪微相互层。在中期气候变化旋回下，主洪水期持续时间长、规模大，沉积分布广泛,形成较厚的灰色水道砂岩沉积和灰色泥岩沉积夹薄层的红色泥坪沉积，间洪水期沉积为砂坪、混合坪与泥坪互层构成。长期旋回表现为每个中期主洪水期越来越小、水道沉积规模变小，间洪水期形成的红色泥坪厚度逐渐加厚，代表气候越来越干旱。研究区的这种地层旋回变化特征反映出气候是地层旋回的主控因素，不仅控制地层的短期旋回，同时控制地层的中长期旋回。这些特征具明显的等时性和可对比性，为油田开发过程中小层对比及油层划分提供了理论依据。

English Abstract

Characteristics of Lacustrine Highresolution Sequence Stratigraphy underArid Climate : a case study of Yuyang Formation (Late Cretaceous) in Southwest of Jianghan Basin

CHEN Bo

Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education, Yangtze University Jingzhou, Hubei 434023

Corresponding author: CHEN Bo

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2007-02-10

Keywords:

Abstract: The sequence in Yuyang Formation of lateCretaceous in southwest of Jianghan Basin is controlled by arid climate. Due to the evolution of climate, the flood period and interflood period alternately occur. In shortterm cycle, the sandstone of channel microfacies and sandflat microfacies deposits in flood period and the mudstone of mudflat microfacies deposits in interflood period. In midterm cycle, there appear several assemblages of shortterm sequence cycle. The main flood period usually lasts quite a long time with a large scale, so there deposits a set of thick grey sandstone of channel microfacies and mudstone of distal microfacies with interlayers of laminar red mudstone of mudflat microfacies .Moreover, there is a set of sandflat, mixedflat and mudflat microfacies in the main interflood period. Different from the two cycles above, in longterm cycle, it has a trend that the scales of the channel decrease in main flood period while the thicknesses of red mudflat increase in interflood period. All these characters in mid& longterm sequence cycle suggest the climate has a tendency to become more and more arid. In terms of the characters of sequences and microfacies in arid climate evolution, the authors build up a set of highresolution stratigraphic sequence and make the stratigraphic correlation.

陈波. 干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例[J]. 沉积学报, 2007, 25(1): 21-28.

引用本文:

陈波. 干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例[J]. 沉积学报, 2007, 25(1): 21-28.

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干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例

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陈波

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Characteristics of Lacustrine Highresolution Sequence Stratigraphy underArid Climate : a case study of Yuyang Formation (Late Cretaceous) in Southwest of Jianghan Basin

Corresponding author: CHEN Bo

计量

目录

干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例

油气资源与勘探技术教育部重点实验室长江大学地球科学学院湖北荆州 434023

通讯作者: 陈波

English Abstract

Characteristics of Lacustrine Highresolution Sequence Stratigraphy underArid Climate : a case study of Yuyang Formation (Late Cretaceous) in Southwest of Jianghan Basin

Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education, Yangtze University Jingzhou, Hubei 434023

Corresponding author: CHEN Bo

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干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例

通讯作者: 陈 波

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Characteristics of Lacustrine Highresolution Sequence Stratigraphy underArid Climate : a case study of Yuyang Formation (Late Cretaceous) in Southwest of Jianghan Basin

Corresponding author: CHEN Bo

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出版历程

目录

干旱气候条件下陆相高分辨层序地层特征研究——以江汉盆地西南缘晚白垩世渔洋组为例

油气资源与勘探技术教育部重点实验室 长江大学地球科学学院 湖北荆州 434023

通讯作者: 陈 波

English Abstract

Characteristics of Lacustrine Highresolution Sequence Stratigraphy underArid Climate : a case study of Yuyang Formation (Late Cretaceous) in Southwest of Jianghan Basin

Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education, Yangtze University Jingzhou, Hubei 434023

Corresponding author: CHEN Bo

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通讯作者:
陈波

油气资源与勘探技术教育部重点实验室长江大学地球科学学院湖北荆州 434023

通讯作者: 陈波