四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境

赵永胜; 王多义; 胡志水

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四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境

赵永胜, 王多义, 胡志水

文章导航 > 沉积学报 > 1994 > 12(2): 1-9

赵永胜, 王多义, 胡志水. 四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境[J]. 沉积学报, 1994, 12(2): 1-9.

引用本文:

赵永胜, 王多义, 胡志水. 四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境[J]. 沉积学报, 1994, 12(2): 1-9.

Zhao Yongsheng, Wang Duoyi, Hu Zhishui. Sedimentology and Environment of Carbonate Gravity- Flows on the Wester Margin of Lower Triassic. Sichuan Basin.[J]. Acta Sedimentologica Sinica, 1994, 12(2): 1-9.

Citation:

Zhao Yongsheng, Wang Duoyi, Hu Zhishui. Sedimentology and Environment of Carbonate Gravity- Flows on the Wester Margin of Lower Triassic. Sichuan Basin.[J]. Acta Sedimentologica Sinica, 1994, 12(2): 1-9.

赵永胜, 王多义, 胡志水. 四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境[J]. 沉积学报, 1994, 12(2): 1-9.

引用本文:

赵永胜, 王多义, 胡志水. 四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境[J]. 沉积学报, 1994, 12(2): 1-9.

Citation:

四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境

成都理工学院石油系

详细信息

作者简介:
赵永胜男 29岁讲师石油地质与勘探(含油区沉积和储层沉积学)

中图分类号: P512.2

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文章访问数: 512
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Sedimentology and Environment of Carbonate Gravity- Flows on the Wester Margin of Lower Triassic. Sichuan Basin.

Chengdu Institute of Technology

摘要

摘要: 四川竹园坝?梨园里地区下三叠统飞仙关组地层中,碳酸盐砾屑沉积类型有:碎屑流和浊流;根据岩性组合可分三种组合层序:Ⅰ.碎屑流与半深水泥晶灰岩沉积组合层序;Ⅱ.碎屑流与浊流沉积组合层序;Ⅲ.复合层序?据重力流形成环境,计算了古斜坡坡度,测定了古流向,结合重力流形成及古构造?古地理演化,提出了区内碳酸盐重力流的演化及沉积模式?
- 碳酸盐重力流 /
- 组合层序 /
- 古斜坡坡度 /
- 演化及模式 /
- 早三叠世 /
- 四川盆地
Abstract: Deposits of carbonate gravity flows on the western margin of Lower Triassic Sichuan bsain may be divided into two parts : debris current and turbidity current. Debris current deposits mainly consist of four kinds of calcirudites with 1. horizontal structure ( type A ),2. graded structure ( type B ),3. disorder fabric (type C),4. matrix supported (type D). Turbidity current deposits are composed of 1. calcarenite for low density current, 2. containcalcirudite calcarenite for high dentity current. Distribution frequency curves of carbonate gravity flow deposits may be classified into four groups. It's importantly disscured differing from curves of debris and turibidity current and varying with their characteristic parameters. Assocaition sequences of gravity flow sediments may show origin and evolution of gravity flow deposits. The association sequences are as follows:1. association with debris flow deposits and micritic limestone in half-deep water environment. 2. association with cohesive debris current(type D) and turbulent debris current(type A B C). 3. association with debris current and turbidity current deposits. 4. complex association with calcilutite-debris current-turbidity current-calcilutite deposits. 1t' s studied that paleo-slope is along northeast-southwest. It dipsfo the is southeast. direction of gravity flow is from northwest to southeast. Its slope angle is about 2-9. Gravity flow deposits have linear distribution. It' s non-water channel gravity flow deposits controlled by a marginal growth fault on the background of plateform geosyncline.
- Carbonate gravity flow /
- paleo-slope angle /
- Lower triassic epoch /
- Association sequence /
- Evolution and model of gravity flow. /

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参考文献(6)

[1]	Hiscott,R. N. and James, N. P.，1985,Carbonate Debris flows. Cow Head Group Western Newfoundland. J.Sedim. Petrol. Vol. 55 p. 735-745.
[2]	Johnson, A. M.，1970, Physical Processes in Geology. Freeman,Cooper and Company, San Francisco.
[3]	l.owe, D. R.，1982, Sediment gravity flows I.Depositional models of high density turbidity currents. J.Sedim. Petrol. Vo1..52, p. 279-297.
[4]	Lowe, D. R.，1976, Grain flow and grain-flow deposits. J. Sedim. Petrol. Vol. 46,p. 188-199.
[5]	Rodine, J. D. and Johnson.M.，1976，The ability of debris heavily freighted with coarse clastic material to flow on gentle slopes. Sedimentology, Vol. 23,p. 213-234.
[6]	Todd, S. P.，1989, Str~-driven, high-density gravelly traction Carpets, possible deposits in the Trabeg Conglomerate Formation, SW. Ireland and some theiroticae consiclerations of their origin. Sedimentology, Vol.36,p. 513-530.

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文章访问数: 512
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四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境

成都理工学院石油系

作者简介:
赵永胜男 29岁讲师石油地质与勘探(含油区沉积和储层沉积学)

刊出日期: 1994-06-10

中图分类号: P512.2

关键词:

摘要: 四川竹园坝?梨园里地区下三叠统飞仙关组地层中,碳酸盐砾屑沉积类型有:碎屑流和浊流;根据岩性组合可分三种组合层序:Ⅰ.碎屑流与半深水泥晶灰岩沉积组合层序;Ⅱ.碎屑流与浊流沉积组合层序;Ⅲ.复合层序?据重力流形成环境,计算了古斜坡坡度,测定了古流向,结合重力流形成及古构造?古地理演化,提出了区内碳酸盐重力流的演化及沉积模式?

English Abstract

Sedimentology and Environment of Carbonate Gravity- Flows on the Wester Margin of Lower Triassic. Sichuan Basin.

Chengdu Institute of Technology

Publish Date: 1994-06-10

Keywords:

Abstract: Deposits of carbonate gravity flows on the western margin of Lower Triassic Sichuan bsain may be divided into two parts : debris current and turbidity current. Debris current deposits mainly consist of four kinds of calcirudites with 1. horizontal structure ( type A ),2. graded structure ( type B ),3. disorder fabric (type C),4. matrix supported (type D). Turbidity current deposits are composed of 1. calcarenite for low density current, 2. containcalcirudite calcarenite for high dentity current. Distribution frequency curves of carbonate gravity flow deposits may be classified into four groups. It's importantly disscured differing from curves of debris and turibidity current and varying with their characteristic parameters. Assocaition sequences of gravity flow sediments may show origin and evolution of gravity flow deposits. The association sequences are as follows:1. association with debris flow deposits and micritic limestone in half-deep water environment. 2. association with cohesive debris current(type D) and turbulent debris current(type A B C). 3. association with debris current and turbidity current deposits. 4. complex association with calcilutite-debris current-turbidity current-calcilutite deposits. 1t' s studied that paleo-slope is along northeast-southwest. It dipsfo the is southeast. direction of gravity flow is from northwest to southeast. Its slope angle is about 2-9. Gravity flow deposits have linear distribution. It' s non-water channel gravity flow deposits controlled by a marginal growth fault on the background of plateform geosyncline.

赵永胜, 王多义, 胡志水. 四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境[J]. 沉积学报, 1994, 12(2): 1-9.

引用本文:

赵永胜, 王多义, 胡志水. 四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境[J]. 沉积学报, 1994, 12(2): 1-9.

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四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境

作者简介:
赵永胜男 29岁讲师石油地质与勘探(含油区沉积和储层沉积学)

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Sedimentology and Environment of Carbonate Gravity- Flows on the Wester Margin of Lower Triassic. Sichuan Basin.

计量

目录

四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境

成都理工学院石油系

作者简介:
赵永胜男 29岁讲师石油地质与勘探(含油区沉积和储层沉积学)

English Abstract

Sedimentology and Environment of Carbonate Gravity- Flows on the Wester Margin of Lower Triassic. Sichuan Basin.

Chengdu Institute of Technology

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四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境

作者简介: 赵永胜 男 29岁 讲师 石油地质与勘探(含油区沉积和储层沉积学)

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Sedimentology and Environment of Carbonate Gravity- Flows on the Wester Margin of Lower Triassic. Sichuan Basin.

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出版历程

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四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境

成都理工学院石油系

作者简介: 赵永胜 男 29岁 讲师 石油地质与勘探(含油区沉积和储层沉积学)

English Abstract

Sedimentology and Environment of Carbonate Gravity- Flows on the Wester Margin of Lower Triassic. Sichuan Basin.

Chengdu Institute of Technology

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目录

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期刊在线

联系我们

作者简介:
赵永胜男 29岁讲师石油地质与勘探(含油区沉积和储层沉积学)

作者简介:
赵永胜男 29岁讲师石油地质与勘探(含油区沉积和储层沉积学)