苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究

舒 强

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苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究

舒强

文章导航 > 沉积学报 > 2006 > 24(2): 276-281

舒强. 苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究[J]. 沉积学报, 2006, 24(2): 276-281.

引用本文:

舒强. 苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究[J]. 沉积学报, 2006, 24(2): 276-281.

SHU Qiang. A Correlation between Magnetic Susceptibility and the Content of Different Grain Sizes of XH1# Core in North Jiangsu Basin and Its Significance[J]. Acta Sedimentologica Sinica, 2006, 24(2): 276-281.

Citation:

SHU Qiang. A Correlation between Magnetic Susceptibility and the Content of Different Grain Sizes of XH1# Core in North Jiangsu Basin and Its Significance[J]. Acta Sedimentologica Sinica, 2006, 24(2): 276-281.

舒强. 苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究[J]. 沉积学报, 2006, 24(2): 276-281.

引用本文:

舒强. 苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究[J]. 沉积学报, 2006, 24(2): 276-281.

Citation:

苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究

舒强

南京师范大学地理科学学院江苏省环境演变与生态建设重点实验室南京 210097

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A Correlation between Magnetic Susceptibility and the Content of Different Grain Sizes of XH1# Core in North Jiangsu Basin and Its Significance

SHU Qiang

.College of Geography Science, Nanjing Normal University, Key Laboratory of Environmental Evolution and Ecological Construction of Jiangsu Province, Nanjing 210097;

More Information

Corresponding author: SHU Qiang

摘要

摘要: 对苏北盆地XH1#钻孔沉积物磁化率与粒度组分的相关性进行了研究，研究结果表明，此钻孔沉积物磁化率与粒度组分的相关性在不同深度段内有着不同的表现：在350～247 m深度段内，磁化率大小与中值粒径大小表现为负相关、与4～12Φ各粒级组分百分含量表现为正相关；在234～0 m深度段内，磁化率大小与中值粒径大小表现为正相关，与1～3Φ粒级组分百分含量表现为密切的正相关；247～234 m深度段是上述两种相关性变化的一个过渡阶段。环境磁学实验结果也揭示出在上下两个深度段内磁性矿物组成上也存在差异。这种不同深度段内磁化率与粒度组分相关性上的大的变化，以及磁性矿物组成上的差异共同揭示出，在深度247～234 m这段沉积物的沉积过程中，苏北盆地内可能发生了一次重大的事件，正是这次重大事件的发生导致了碎屑沉积物来源的改变，出现了上下两部分磁化率大小与粒度组分相关性上的差异。
- 磁化率 /
- 粒度 /
- 相关性 /
- 苏北盆地
Abstract: Based on the synthetic study on the correlations between magnetic susceptibility and the content of the different grain size〖KG*2〗of XH1# core in northern Jiangsu basin, this paper shows that the correlation is different〖KG*2〗in various depth: 350~247m, the mass susceptibility correlates negatively with〖KG*2〗mid-grain sizes, but correlates positively with the content〖KG*2〗of 4~12Φ; 234~0m, the mass susceptibility correlates positively with〖KG*2〗mid-grain sizes, and correlates positively with the content〖KG*2〗of 1~3Φ; The depth of 247~234m is the transition period of the transform of the correlations between magnetic susceptibility and the content of the different grain size.〖KG*2〗The results of environmental magnetism research〖KG*2〗show that the components〖KG*2〗of magnetic mineral are also different〖KG*2〗in the upper stratum(234~0m) and the lower stratum(350~247m). The difference〖KG*2〗of the correlations between magnetic susceptibility and the content of the different grain size,〖KG*2〗and the components〖KG*2〗of magnetic mineral in various depth reveal that, in the course〖KG*2〗of the sediment deposition in the depth 247~234m, one great event may have happened in Northern Jiangsu Basin, this event led to the change of detrital sediment〖KG*2〗origin.
- susceptibility /
- grain size /
- correlation /
- northern Jiangsu basin

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[1]	乔大伟, 王红亮. 基于粒度小波变换分析的四川盐源盆地沉积特征及其对盆地形成演化的指示意义 . 沉积学报, 2019, 37(4): 713-722. doi: 10.14027/j.issn.1000-0550.2018.165
[2]	刘建宁, 董桂玉, 王兵杰, 张琳婷, 霍少川, 曹玉鹏, 彭凯, 冷春鹏. 苏北盆地高邮凹陷戴南组震积岩特征及其石油地质意义 . 沉积学报, 2018, 36(6): 1267-1276. doi: 10.14027/j.issn.1000-0550.2018.095
[3]	滕晓华, 张志高, 韩文霞, 方亚会, 叶程程. 塔里木盆地南缘黄土粒度特征及其环境意义 . 沉积学报, 2015, 33(5): 941-950. doi: 10.14027/j.cnki.cjxb.2015.05.010
[4]	. 北京市昌平区钻孔岩芯的磁化率与粒度组份变化的相关性研究 . 沉积学报, 2012, 30(3): 572-579.
[5]	田庆春. 青藏高原腹地湖泊沉积物磁化率及其环境意义 . 沉积学报, 2011, 29(1): 143-150.
[6]	闫晓丽. 临夏盆地黑林顶剖面沉积物在8.6Ma前后岩石磁学特征及其意义 . 沉积学报, 2010, 28(6): 1190-1197.
[7]	周健. 苏北盆地高邮凹陷马家嘴地区古近系戴南组物源分析 . 沉积学报, 2010, 28(6): 1117-1128.
[8]	杨黎静. 台湾海峡西部表层沉积物磁化率特征 . 沉积学报, 2009, 27(4): 697-703.
[9]	舒强. 苏北盆地浅钻沉积物磁化率与粒度记录的末次冰消期以来的环境变化 . 沉积学报, 2009, 27(1): 111-117.
[10]	赵军. 东秦岭地区黄土堆积的岩石磁学特征及磁化率增强机制探索 . 沉积学报, 2008, 26(6): 1052-1062.
[11]	傅强. 苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义 . 沉积学报, 2007, 25(3): 380-385.
[12]	张喜林. 苏北盆地高邮凹陷古近系戴南组滨浅湖沉积中的遗迹化石 . 沉积学报, 2006, 24(1): 81-89.
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[14]	龙昱, 李永涛, 李晓. 武汉东湖现代沉积界面时间标定的磁化率与工业事件分析 . 沉积学报, 2002, 20(3): 421-426.
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苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究

舒强

南京师范大学地理科学学院江苏省环境演变与生态建设重点实验室南京 210097

通讯作者: 舒强

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2006-04-10

关键词:

磁化率 /

粒度 /

English Abstract

A Correlation between Magnetic Susceptibility and the Content of Different Grain Sizes of XH1# Core in North Jiangsu Basin and Its Significance

SHU Qiang

.College of Geography Science, Nanjing Normal University, Key Laboratory of Environmental Evolution and Ecological Construction of Jiangsu Province, Nanjing 210097;

Corresponding author: SHU Qiang

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2006-04-10

Keywords:

Abstract: Based on the synthetic study on the correlations between magnetic susceptibility and the content of the different grain size〖KG*2〗of XH1# core in northern Jiangsu basin, this paper shows that the correlation is different〖KG*2〗in various depth: 350~247m, the mass susceptibility correlates negatively with〖KG*2〗mid-grain sizes, but correlates positively with the content〖KG*2〗of 4~12Φ; 234~0m, the mass susceptibility correlates positively with〖KG*2〗mid-grain sizes, and correlates positively with the content〖KG*2〗of 1~3Φ; The depth of 247~234m is the transition period of the transform of the correlations between magnetic susceptibility and the content of the different grain size.〖KG*2〗The results of environmental magnetism research〖KG*2〗show that the components〖KG*2〗of magnetic mineral are also different〖KG*2〗in the upper stratum(234~0m) and the lower stratum(350~247m). The difference〖KG*2〗of the correlations between magnetic susceptibility and the content of the different grain size,〖KG*2〗and the components〖KG*2〗of magnetic mineral in various depth reveal that, in the course〖KG*2〗of the sediment deposition in the depth 247~234m, one great event may have happened in Northern Jiangsu Basin, this event led to the change of detrital sediment〖KG*2〗origin.

舒强. 苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究[J]. 沉积学报, 2006, 24(2): 276-281.

引用本文:

舒强. 苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究[J]. 沉积学报, 2006, 24(2): 276-281.

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苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究

通讯作者:
舒强

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A Correlation between Magnetic Susceptibility and the Content of Different Grain Sizes of XH1# Core in North Jiangsu Basin and Its Significance

Corresponding author: SHU Qiang

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苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究

南京师范大学地理科学学院江苏省环境演变与生态建设重点实验室南京 210097

通讯作者: 舒强

English Abstract

A Correlation between Magnetic Susceptibility and the Content of Different Grain Sizes of XH1# Core in North Jiangsu Basin and Its Significance

.College of Geography Science, Nanjing Normal University, Key Laboratory of Environmental Evolution and Ecological Construction of Jiangsu Province, Nanjing 210097;

Corresponding author: SHU Qiang

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苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究

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A Correlation between Magnetic Susceptibility and the Content of Different Grain Sizes of XH1# Core in North Jiangsu Basin and Its Significance

Corresponding author: SHU Qiang

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苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究

南京师范大学地理科学学院 江苏省环境演变与生态建设重点实验室 南京 210097

通讯作者: 舒 强

English Abstract

A Correlation between Magnetic Susceptibility and the Content of Different Grain Sizes of XH1# Core in North Jiangsu Basin and Its Significance

.College of Geography Science, Nanjing Normal University, Key Laboratory of Environmental Evolution and Ecological Construction of Jiangsu Province, Nanjing 210097;

Corresponding author: SHU Qiang

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通讯作者:
舒强

南京师范大学地理科学学院江苏省环境演变与生态建设重点实验室南京 210097

通讯作者: 舒强