东营凹陷古近系中深层湖盆演化中的无机元素响应

陈中红

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东营凹陷古近系中深层湖盆演化中的无机元素响应

陈中红

文章导航 > 沉积学报 > 2008 > 26(6): 925-932

陈中红. 东营凹陷古近系中深层湖盆演化中的无机元素响应[J]. 沉积学报, 2008, 26(6): 925-932.

引用本文:

陈中红. 东营凹陷古近系中深层湖盆演化中的无机元素响应[J]. 沉积学报, 2008, 26(6): 925-932.

CHEN Zhonghong. Mineral Elemental Response to the Evolution of Terrestrial Brine Faultedbasin:a case study in the Paleogene of Well Haoke1, Dongying Sag[J]. Acta Sedimentologica Sinica, 2008, 26(6): 925-932.

Citation:

CHEN Zhonghong. Mineral Elemental Response to the Evolution of Terrestrial Brine Faultedbasin:a case study in the Paleogene of Well Haoke1, Dongying Sag[J]. Acta Sedimentologica Sinica, 2008, 26(6): 925-932.

陈中红. 东营凹陷古近系中深层湖盆演化中的无机元素响应[J]. 沉积学报, 2008, 26(6): 925-932.

引用本文:

陈中红. 东营凹陷古近系中深层湖盆演化中的无机元素响应[J]. 沉积学报, 2008, 26(6): 925-932.

Citation:

东营凹陷古近系中深层湖盆演化中的无机元素响应

陈中红

中国石油大学(华东)地球资源与信息学院山东东营 257061)

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陈中红

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Mineral Elemental Response to the Evolution of Terrestrial Brine Faultedbasin:a case study in the Paleogene of Well Haoke1, Dongying Sag

CHEN Zhonghong

China University of Petroleum, Dongying Shandong 257061

More Information

Corresponding author: CHEN Zhonghong

摘要

摘要: 为查明无机元素分布与水深、盐度等沉积环境以及湖盆演化过程的关系，采用电感耦合等离子体发射光谱仪分析对东营凹陷郝科1科探井古近系深层微量元素含量进行了测试、分析，所涉及的研究层位是该凹陷的主要烃源岩层段（沙河街组三亚段、沙河街组四亚段、孔店组），分析结果表明：在水体浅、蒸发作用强烈的孔店组—沙四下亚段强氧化性滨浅湖环境里，钙、锶含量和Ca/Mg、Sr/Ba、Sr/Ca参数值具低值响应，铁、铝、钡、钒含量和（Fe+Al）/(Ca+Mg)参数值具高值响应；在沙四中亚段膏岩、盐岩等普遍发育的盐湖环境中，钠、锶含量和Sr/Ba、Fe/Mn、Sr/Ca均出现高值响应，锰、钡、钒含量和V/Ni、(Fe+Al)/(Ca+Mg)出现低值响应；在还原性的沙四上亚段半咸化深湖环境中，钾、钠、铁含量和Fe/Mn值具低值响应，钙、锰含量具高值响应；在沙四中亚段膏盐与泥岩共生体系中元素分布离散性明显，呈现波动性特征；Sr/Ba、Sr/Ca在盐湖环境中出现显著的高值响应，被证实可以作为良好的水体盐度指标参数，Fe/Mn、(Fe+Al)/(Ca+Mg)随水体加深逐渐增大，是良好的水体深浅指标参数。元素分布受沉积环境、岩性特征等多种地质因素的影响，在利用元素含量分布及特征元素比值来判断某单个地质因素的变化时，应该应用多种参数，进行综合判断。
- 无机元素响应 /
- 元素比值参数 /
- 湖盆演化 /
- 盐湖 /
- 东营凹陷
Abstract: In order to investigate the relation between the distribution of mineral elements and sedimentary environment including the salinity and depth of water body, and the evolution of lakebasin, emission spectrograph of inductive coupling plasma was used to intensively testing and dissection the content of mineral elements in the deep death of the Paleogene from the Well Haoke1 in Dongying sag. The involved formation contained the Member 3, Member 4 of Shahejie Formation and Kongdian Formation, in which the main source rocks distributed. The results demonstrate that: in the oxidized sedimentary environment of shallow shorelacustrine the content of Sr, Ca and the parameters of Ca/Mg, Sr/Ba, Sr/Ca have low value response, the content of Fe, Al, Ba, V and the parameter of (Fe+Al)/(Ca+Mg) have high value response; in the brinelake sedimentary environment the content of Mn, Ba,V and the parameters of V/Ni, (Fe+Al)/(Ca+Mg) have low value response, the content of Sr, Na and the parameters of Sr/Ba, Fe/Mn, Sr/Ca have high value response; in the reductive brackish sedimentary environment of halfdeep lacustrine lake the content of K, Na, Fe and the parameters of Fe/Mn have low value response, the content of Ca, Mn have high value response. In the cosedimentary environment of saline deposit and mud of the middle part of Sha4 Formation, the distribution of mineral elements has obvious characteristics of discretion and fluctuation. Sr/Ba, Sr/Ca have obvious high value response in the saline lake and are verified to be good parameters for salinity of waterbody. The parameters of Fe/Mn and (Fe+Al)/(Ca+Mg) are approved to be good parameters for the depth of waterbody and their value increased with deepening of waterbody. The parameters abovementioned should be applied and synthetically analyzed to determine characteristics of geological factors for the parameters were influenced by many geological factors including sedimentary environment and lithologic character. 
- response of mineral element /
- ratio of mineral element /
- evolution of basin /
- brine lake /
- Dongying Sag

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[1]	王健, 彭捷, 操应长, 刘可禹, 宋明水, 刘惠民. 东营凹陷中晚始新世古气候演化特征及其意义——以Hk1井为例 . 沉积学报, 2022, 40(4): 1059-1072. doi: 10.14027/j.issn.1000-0550.2021.010
[2]	. 食盐析出实验对盐湖盆地沉积研究的启示 . 沉积学报, 2014, 32(2): 238-243.
[3]	吴旭东. 全新世低纬地区古环境演化与北大西洋之间的联系——以湖光岩玛珥湖元素和元素比值记录为例 . 沉积学报, 2011, 29(5): 926-934.
[4]	陈中红. 东营凹陷古近系升藿烷生物标志物参数分布及演变规律 . 沉积学报, 2011, 29(1): 173-183.
[5]	陈中红. 典型断陷湖盆C27三降藿烷参数演化及其控制因素——以东营凹陷古近系为例〖 . 沉积学报, 2010, 28(3): 635-642.
[6]	操应长. 东营凹陷西部沙四上亚段滩坝砂体有效储层的物性下限及控制因素 . 沉积学报, 2009, 27(2): 230-237.
[7]	李明慧. 青藏高原秋里南木湖原生硼砂、芒硝韵律层的发现及气候环境意义 . 沉积学报, 2007, 25(4): 619-625.
[8]	袁静. 东营凹陷深层溶蚀孔隙的多重介质成因机理和动力机制 . 沉积学报, 2007, 25(6): 840-846.
[9]	操应长. 特征元素比值在沉积物物源分析中的应用——以东营凹陷王58井区沙四上亚段研究为例 . 沉积学报, 2007, 25(2): 230-238.
[10]	赵全民, 杨道庆, 江继刚, 彭江, 徐士忠. 舞阳、襄城凹陷下第三系盐湖相有机地球化学与沉积环境研究 . 沉积学报, 2003, 21(2): 334-339.
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[14]	李玉梅, 赵澄林. 盐湖盆地斜坡带碎屑岩成岩作用特征初探──以柴达木盆地阿尔金斜坡第三系碎屑岩地层为例 . 沉积学报, 1998, 16(1): 126-131.
[15]	王随继, 黄杏珍, 妥进才, 邵宏舜, 阎存凤, 王寿庆, 何祖荣. 泌阳凹陷核桃园组微量元素演化特征及其古气候意义 . 沉积学报, 1997, 15(1): 65-70.
[16]	刘兴起, 于升松, 邵明昱. 察尔汗盐湖碎屑沉积元素地层学的初步研究 . 沉积学报, 1997, 15(S1): 142-146.
[17]	江德昕, 魏俊超. 内蒙古查干诺尔盐湖晚更新世至全新世孢粉植物群与古气候 . 沉积学报, 1997, 15(S1): 147-151.
[18]	妥进才, 邵宏舜, 黄杏珍. 盐湖相生油岩中某些地球化学参数与沉积环境的关系 . 沉积学报, 1994, 12(3): 114-119.
[19]	张水昌, 黄汝昌, 于心科. 盐湖盆地沉积有机质中的脱羟基维生素E . 沉积学报, 1990, 8(1): 57-64.
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东营凹陷古近系中深层湖盆演化中的无机元素响应

陈中红

中国石油大学(华东)地球资源与信息学院山东东营 257061)

通讯作者: 陈中红

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2008-12-10

关键词:

盐湖 /

摘要: 为查明无机元素分布与水深、盐度等沉积环境以及湖盆演化过程的关系，采用电感耦合等离子体发射光谱仪分析对东营凹陷郝科1科探井古近系深层微量元素含量进行了测试、分析，所涉及的研究层位是该凹陷的主要烃源岩层段（沙河街组三亚段、沙河街组四亚段、孔店组），分析结果表明：在水体浅、蒸发作用强烈的孔店组—沙四下亚段强氧化性滨浅湖环境里，钙、锶含量和Ca/Mg、Sr/Ba、Sr/Ca参数值具低值响应，铁、铝、钡、钒含量和（Fe+Al）/(Ca+Mg)参数值具高值响应；在沙四中亚段膏岩、盐岩等普遍发育的盐湖环境中，钠、锶含量和Sr/Ba、Fe/Mn、Sr/Ca均出现高值响应，锰、钡、钒含量和V/Ni、(Fe+Al)/(Ca+Mg)出现低值响应；在还原性的沙四上亚段半咸化深湖环境中，钾、钠、铁含量和Fe/Mn值具低值响应，钙、锰含量具高值响应；在沙四中亚段膏盐与泥岩共生体系中元素分布离散性明显，呈现波动性特征；Sr/Ba、Sr/Ca在盐湖环境中出现显著的高值响应，被证实可以作为良好的水体盐度指标参数，Fe/Mn、(Fe+Al)/(Ca+Mg)随水体加深逐渐增大，是良好的水体深浅指标参数。元素分布受沉积环境、岩性特征等多种地质因素的影响，在利用元素含量分布及特征元素比值来判断某单个地质因素的变化时，应该应用多种参数，进行综合判断。

English Abstract

Mineral Elemental Response to the Evolution of Terrestrial Brine Faultedbasin:a case study in the Paleogene of Well Haoke1, Dongying Sag

CHEN Zhonghong

China University of Petroleum, Dongying Shandong 257061

Corresponding author: CHEN Zhonghong

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2008-12-10

Keywords:

Abstract: In order to investigate the relation between the distribution of mineral elements and sedimentary environment including the salinity and depth of water body, and the evolution of lakebasin, emission spectrograph of inductive coupling plasma was used to intensively testing and dissection the content of mineral elements in the deep death of the Paleogene from the Well Haoke1 in Dongying sag. The involved formation contained the Member 3, Member 4 of Shahejie Formation and Kongdian Formation, in which the main source rocks distributed. The results demonstrate that: in the oxidized sedimentary environment of shallow shorelacustrine the content of Sr, Ca and the parameters of Ca/Mg, Sr/Ba, Sr/Ca have low value response, the content of Fe, Al, Ba, V and the parameter of (Fe+Al)/(Ca+Mg) have high value response; in the brinelake sedimentary environment the content of Mn, Ba,V and the parameters of V/Ni, (Fe+Al)/(Ca+Mg) have low value response, the content of Sr, Na and the parameters of Sr/Ba, Fe/Mn, Sr/Ca have high value response; in the reductive brackish sedimentary environment of halfdeep lacustrine lake the content of K, Na, Fe and the parameters of Fe/Mn have low value response, the content of Ca, Mn have high value response. In the cosedimentary environment of saline deposit and mud of the middle part of Sha4 Formation, the distribution of mineral elements has obvious characteristics of discretion and fluctuation. Sr/Ba, Sr/Ca have obvious high value response in the saline lake and are verified to be good parameters for salinity of waterbody. The parameters of Fe/Mn and (Fe+Al)/(Ca+Mg) are approved to be good parameters for the depth of waterbody and their value increased with deepening of waterbody. The parameters abovementioned should be applied and synthetically analyzed to determine characteristics of geological factors for the parameters were influenced by many geological factors including sedimentary environment and lithologic character. 

陈中红. 东营凹陷古近系中深层湖盆演化中的无机元素响应[J]. 沉积学报, 2008, 26(6): 925-932.

引用本文:

陈中红. 东营凹陷古近系中深层湖盆演化中的无机元素响应[J]. 沉积学报, 2008, 26(6): 925-932.

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东营凹陷古近系中深层湖盆演化中的无机元素响应

通讯作者:
陈中红

计量

Mineral Elemental Response to the Evolution of Terrestrial Brine Faultedbasin:a case study in the Paleogene of Well Haoke1, Dongying Sag

Corresponding author: CHEN Zhonghong

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东营凹陷古近系中深层湖盆演化中的无机元素响应

中国石油大学(华东)地球资源与信息学院山东东营 257061)

通讯作者: 陈中红

English Abstract

Mineral Elemental Response to the Evolution of Terrestrial Brine Faultedbasin:a case study in the Paleogene of Well Haoke1, Dongying Sag

China University of Petroleum, Dongying Shandong 257061

Corresponding author: CHEN Zhonghong

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东营凹陷古近系中深层湖盆演化中的无机元素响应

通讯作者: 陈中红

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Mineral Elemental Response to the Evolution of Terrestrial Brine Faultedbasin:a case study in the Paleogene of Well Haoke1, Dongying Sag

Corresponding author: CHEN Zhonghong

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东营凹陷古近系中深层湖盆演化中的无机元素响应

中国石油大学(华东)地球资源与信息学院 山东东营 257061)

通讯作者: 陈中红

English Abstract

Mineral Elemental Response to the Evolution of Terrestrial Brine Faultedbasin:a case study in the Paleogene of Well Haoke1, Dongying Sag

China University of Petroleum, Dongying Shandong 257061

Corresponding author: CHEN Zhonghong

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通讯作者:
陈中红

中国石油大学(华东)地球资源与信息学院山东东营 257061)