辽河盆地西部凹陷粘土矿物的成岩作用研究

陈永武; 任磊夫

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辽河盆地西部凹陷粘土矿物的成岩作用研究

陈永武, 任磊夫

文章导航 > 沉积学报 > 1985 > 3(3): 51-64

陈永武, 任磊夫. 辽河盆地西部凹陷粘土矿物的成岩作用研究[J]. 沉积学报, 1985, 3(3): 51-64.

引用本文:

陈永武, 任磊夫. 辽河盆地西部凹陷粘土矿物的成岩作用研究[J]. 沉积学报, 1985, 3(3): 51-64.

Cheng Yongwu, Ren Leifu. STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN[J]. Acta Sedimentologica Sinica, 1985, 3(3): 51-64.

Citation:

Cheng Yongwu, Ren Leifu. STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN[J]. Acta Sedimentologica Sinica, 1985, 3(3): 51-64.

陈永武, 任磊夫. 辽河盆地西部凹陷粘土矿物的成岩作用研究[J]. 沉积学报, 1985, 3(3): 51-64.

引用本文:

陈永武, 任磊夫. 辽河盆地西部凹陷粘土矿物的成岩作用研究[J]. 沉积学报, 1985, 3(3): 51-64.

Cheng Yongwu, Ren Leifu. STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN[J]. Acta Sedimentologica Sinica, 1985, 3(3): 51-64.

Citation:

Cheng Yongwu, Ren Leifu. STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN[J]. Acta Sedimentologica Sinica, 1985, 3(3): 51-64.

辽河盆地西部凹陷粘土矿物的成岩作用研究

陈永武¹,
任磊夫²

1.
石油勘探开发科学研究院地质所;
2.
北京大学

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文章访问数: 480
HTML全文浏览量: 8
PDF下载量: 419
被引次数: 0

STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN

Cheng Yongwu¹,
Ren Leifu²

1.
C Scientific Research Institute of Petroleum Exploration and Development, Beijing;
2.
Peking University

摘要

摘要: 对辽河盆地西部凹陷兴隆台、马圈子、欢喜岭和曙光等地沙河街组不同深度的层位,高升地区(属弱碱性和弱氧化—弱还原环境的沙四段分别采样,经X-光衍射、电子显微镜、化学分析和差热、红外等项目的分析鉴定,研究区内的粘土矿物有: 蒙脱石在全区较浅的地层(如欢喜岭地区小于1000米,兴隆台地区小于1500米)中均有分布。其主要成份为二八面体的钙蒙脱石。皂石为黑色橄榄-辉石玄武岩的次生产物。

Abstract: Different clay mineral assemblages and their replacement have been formed in different sedimentary and diagenetic environments in the western depression ( Huan-xiling, Xinglongtai and Maquanzhi ): 1.Montmorillonite-I/M-illite-kaolinite mineral assemblage 2.1/M-authigenic illite-atlthigenic chiorite mineral assemblage The weak acidic and weak alkaline environments were transformed into slight alkaine-weak reductive ones with the increase of depth and geothermal and mont-morillonite and I/M turned into illite and trioctahedron chlorite. In the north region of the western depression ( Gaosheng and the local area of Shuguang)t 1. I/M-illie mineral assemblage 2. Glauconite-trioctahedron smectite mineral assemblage 3. Fe-saponite mineral The Sha-4 stage in the area was a slight alkaline-weak reductive sedimentary environment without kaolinite mineral and Ca, Fe3 + Fe2+and Mg were rich in the environment due to the degeneration of the secondary saponite from basalt into trio-dioctahedron smectite. Together with Fe and Mg, K and Al supplied by solubilized K and Al-bearing terrigenous minerals under the higher geothermal moved into I/M crystal lattices and thus forming glauconite. The evidence of mineralogy has shown that the geochemical properties of the sedimentary and diagenetic environments are the principal factors which control low-temperature geochemial behaviors of clay minerals during the diagenesis, and secondly, the temperature also plays an important part during the diagenesis of clay minerals.

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参考文献(1)

[1]

(1) Joaas, E. C, and Brown, T, E,，1959: Analysis of iaterlayer mixtures of three clay miaeraltypes by x-ray differaction. Jour. Sedi. Petrol, Vol. 29, pp77-86.

(2)Fairbrige, R. W, and Bourgeors, J.，1978: The encyclopedia of sedimentology. Encyclopedia of earth science, Vol, V1. pp149-156,

(3)Grim, R, E, and Kulbicki, G,，1961, Montmorilloaite, High temperature reac-tioas and classification. Am, Miner. Yol, 46, pp1329-1389.

(4)Grim. R, E,，Bray, R. H. and Bradley, W. F.，193?: The mica in argilleceus sediments. Am, Miner. Vol, 22, pp813-829,

(5)Kodama,H.and Dean,R.S.，1980,lllise from Eldorao,Sask-atchewan TheCanadianminer.Vol18,Pat.l,pp109-118

(6)Weaver. C, E, and Pollard, L, D.，1973: The chemistry of clay minerals deve-lopments in

(7)Porrenga, D. H.，1968s Non-marine glauconitic illite in the lower Oligocence of Aardeburg, Belgium. Clay Miner. Vol. 7，pp421-430.

(8)Rex, R, W,，1964, Athigenic kaolinite and mica as evidence for phase equilibria at low temperature.Clays and Clay Miner, Proc, of the thirteenth national confer- ence on and Clay minerals, pp, 95-104,

(9)Divis, A, F, and Mckenaie, J. A.，1975: Experimental authigenesis of phyllosi-llicate from feldspathic sands. Sedimentology Vol. 22, pp147-155.

(10)Hoffman, J. and Hower, J,，1979: Clay mineral assemblages as low grade meta- morphic geothermometr, application to the thrust faulted disturbed belt of Mon- tana, U. S, A,

(11)Veld, B,，1977: Clays and clay minerals in nature and sythet'ic system Develop- meats. in sedimentoloyg 21 pp54-59.

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辽河盆地西部凹陷粘土矿物的成岩作用研究

陈永武¹,
任磊夫²

1. 石油勘探开发科学研究院地质所;

2. 北京大学

收稿日期: 1983-11-19
刊出日期: 1985-09-10

摘要: 对辽河盆地西部凹陷兴隆台、马圈子、欢喜岭和曙光等地沙河街组不同深度的层位,高升地区(属弱碱性和弱氧化—弱还原环境的沙四段分别采样,经X-光衍射、电子显微镜、化学分析和差热、红外等项目的分析鉴定,研究区内的粘土矿物有: 蒙脱石在全区较浅的地层(如欢喜岭地区小于1000米,兴隆台地区小于1500米)中均有分布。其主要成份为二八面体的钙蒙脱石。皂石为黑色橄榄-辉石玄武岩的次生产物。

English Abstract

STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN

Cheng Yongwu¹,
Ren Leifu²

1. C Scientific Research Institute of Petroleum Exploration and Development, Beijing;

2. Peking University

Received Date: 1983-11-19
Publish Date: 1985-09-10

Abstract: Different clay mineral assemblages and their replacement have been formed in different sedimentary and diagenetic environments in the western depression ( Huan-xiling, Xinglongtai and Maquanzhi ): 1.Montmorillonite-I/M-illite-kaolinite mineral assemblage 2.1/M-authigenic illite-atlthigenic chiorite mineral assemblage The weak acidic and weak alkaline environments were transformed into slight alkaine-weak reductive ones with the increase of depth and geothermal and mont-morillonite and I/M turned into illite and trioctahedron chlorite. In the north region of the western depression ( Gaosheng and the local area of Shuguang)t 1. I/M-illie mineral assemblage 2. Glauconite-trioctahedron smectite mineral assemblage 3. Fe-saponite mineral The Sha-4 stage in the area was a slight alkaline-weak reductive sedimentary environment without kaolinite mineral and Ca, Fe3 + Fe2+and Mg were rich in the environment due to the degeneration of the secondary saponite from basalt into trio-dioctahedron smectite. Together with Fe and Mg, K and Al supplied by solubilized K and Al-bearing terrigenous minerals under the higher geothermal moved into I/M crystal lattices and thus forming glauconite. The evidence of mineralogy has shown that the geochemical properties of the sedimentary and diagenetic environments are the principal factors which control low-temperature geochemial behaviors of clay minerals during the diagenesis, and secondly, the temperature also plays an important part during the diagenesis of clay minerals.

陈永武, 任磊夫. 辽河盆地西部凹陷粘土矿物的成岩作用研究[J]. 沉积学报, 1985, 3(3): 51-64.

引用本文:

陈永武, 任磊夫. 辽河盆地西部凹陷粘土矿物的成岩作用研究[J]. 沉积学报, 1985, 3(3): 51-64.

Cheng Yongwu, Ren Leifu. STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN[J]. Acta Sedimentologica Sinica, 1985, 3(3): 51-64.

Citation:

Cheng Yongwu, Ren Leifu. STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN[J]. Acta Sedimentologica Sinica, 1985, 3(3): 51-64.

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STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN

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辽河盆地西部凹陷粘土矿物的成岩作用研究

1. 石油勘探开发科学研究院地质所;

2. 北京大学

English Abstract

STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN

1. C Scientific Research Institute of Petroleum Exploration and Development, Beijing;

2. Peking University

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STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN

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出版历程

目录

辽河盆地西部凹陷粘土矿物的成岩作用研究

1. 石油勘探开发科学研究院地质所; 2. 北京大学

English Abstract

STUDY ON DIAGENESIS OF CLAY MINERALS IN THE WESTERN DEPRESSION OF THE LIAOHE BASIN

1. C Scientific Research Institute of Petroleum Exploration and Development, Beijing; 2. Peking University

全文HTML

目录

友情链接

期刊在线

联系我们

1. 石油勘探开发科学研究院地质所;

2. 北京大学

1. C Scientific Research Institute of Petroleum Exploration and Development, Beijing;

2. Peking University