济源盆地谭庄组(T<sub>2-3</sub>)上段湖相沉积及遗迹化石特征

张国成; 曾玉凤; Buatois LA; Mangano MG

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济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征

张国成, 曾玉凤, Buatois LA, Mangano MG

文章导航 > 沉积学报 > 2005 > 23(1): 99-107

张国成, 曾玉凤, Buatois LA, Mangano MG. 济源盆地谭庄组(T2-3)上段湖相沉积及遗迹化石特征[J]. 沉积学报, 2005, 23(1): 99-107.

引用本文:

张国成, 曾玉凤, Buatois LA, Mangano MG. 济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征[J]. 沉积学报, 2005, 23(1): 99-107.

ZHANG Guo-cheng, ZENG Yu-feng, Buatois L A, Mangano M G. Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation ( T2-3 ), Jiyuan Basin, Henan Province[J]. Acta Sedimentologica Sinica, 2005, 23(1): 99-107.

Citation:

ZHANG Guo-cheng, ZENG Yu-feng, Buatois L A, Mangano M G. Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation ( T_2-3 ), Jiyuan Basin, Henan Province[J]. Acta Sedimentologica Sinica, 2005, 23(1): 99-107.

张国成, 曾玉凤, Buatois LA, Mangano MG. 济源盆地谭庄组(T2-3)上段湖相沉积及遗迹化石特征[J]. 沉积学报, 2005, 23(1): 99-107.

引用本文:

张国成, 曾玉凤, Buatois LA, Mangano MG. 济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征[J]. 沉积学报, 2005, 23(1): 99-107.

Citation:

济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征

1.
河南理工大学,河南焦作 454100;
2.
Facultad de Ciencias Naturales Universidad Nacional de Tucum an Casilla de Correo 1 (CC) 4000 San Miguel

基金项目: 国家自然科学基金项目(批准号: 40172045);河南省教育厅基金项目(2003170054);焦作工学院博士基金项目(1005921)资助.

详细信息

作者简介:
张国成，男，1964年出生，副教授，博士，沉积大地构造学与遗迹学。

中图分类号: P512.2;Q911

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文章访问数: 632
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Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation ( T_2-3 ), Jiyuan Basin, Henan Province

1.
Henan Polytechnic University,Jiaozuo Henan 454100;
2.
Facultad de Ciencias Naturales Universidad Nacional de Tucuman,Casilla de Correo 1 (CC) 4000 San Miguel

摘要

摘要: 济源市西南郊出露有中—上三叠统谭庄组,代表了济源中生代盆地充填的一部分。在湖相剖面中识别出六种岩相组成的两类相序,相序 1呈叠置的向上变粗的序列,由下到上由富有机质页岩 (相E,类型Ⅰ ),纹层粉砂岩 (相A)和水流波痕层理砂岩(相B)组成,记录了在温暖潮湿条件下常年性开放湖泊中小型河口坝三角洲的进积作用;相序 2缺少明显的垂直序列,由互层状细粒碳酸盐岩和粉砂岩(相C),变形层理和波浪改造砂岩 (相D),富有机质页岩(相E,类型Ⅱ)和粘土岩组成,虽然也代表了常年性开放浅水湖泊体系,但反映出很强的季节性气候控制特征。湖相剖面的相C中发育丰富的Skolithos linearis组合,也反映出底层受季节性气候控制。文章深入探讨了该组上段浅湖沉积的环境演替及气候对沉积作用的控制作用,在湖泊演化过程中,很可能出现过几次水体分层。根据晚三叠世时期的古地理重建,推测谭庄组上段湖相沉积反映出的强烈季节性可以用潘加亚巨型季风影响的设想模式解释。
- 湖相沉积 /
- 遗迹化石 /
- 气候控制 /
- 济源盆地 /
- 谭庄组
Abstract: The Middle to Upper Triassic Tanzhuang Form ation, being well cropped out near Jiyuan City, Henan Province,represents a part of the infill of the earlyMesozoic Jiyuan-Yima Basin. The upper part of this stratigraphic unit records deposition with in prevailing shallow lake conditions. S ix sedim entary facies clustered into two facies assemb lages were recognized in the lacustrine section. Facies assemb lage 1 consists of the stacked coarsening-upward sequences composed, from base to top, of organic-rich shale ( facies E, typeⅠ), laminated siltstones (facies A) and current-rippled laminated sandstones (facies B). Units of assemb lages 1 record progradat ion o f smallmouth-bar de ltas with in a perennial open lacustr ine system under temperate and humid cond itions. Facies assemb lage 2 lacks a clear vertical prograd ition pattern and consists of in terbedded f ine-grained carbonates and siltstones ( facies C ); de formed and wave-rewo rked sandstones ( fac ies D ) ; organic-rich shales ( facies E, type Ⅱ ) and clayey mudstones ( facies F). The assemb lage also represents a perennia,l hydro log ica lly open, shallow lacustrine system, but characterized by strong seasona l climatic control. The Skolithos linearismonospecific assemb lagema in ly occurred abundantly in faciesC suggests the substrates contro lled by seasona l climate. Water strat ification probably occurred in severa l periods of the lake history. Pangaean megamonsoonal influence is env isaged to expla in the strong seasonality imprint evidenced tow ard the upper part of the Tanzhuang lacustrine co lumn.
- lacustrine deposit /
- trace fossil /
- climatic control /
- Jiyuan Basin /
- Tangzhuang Formation

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参考文献(1)

[1]

1 吴贤涛. 豫西济源-义马盆地浊流沉积中的痕迹化石及其环境意义[J].沉积学报,1985,(03):23-31.

2 胡斌,齐永安,张国成. 中国中-新生代陆相沉积中的遗迹群落[J].沉积学报,2002,(04):574-581.

3 康明,孟凡顺,任宝山. 河南省中生代含煤地层的划分和对比[J].焦作矿业学院学报,1985.23-29.

4 胡斌. 豫西济源地区的晚三叠世-中侏罗世陆相地层[J].地层学杂志,1991.48-52.

5 BuatoisLA,Mangano M G,Xiaotao Wu,Guocheng Zhang. Trace fossils from Jurassic lacustrine turbidites of the Anyao Formation central China and their environmental and evolutionary significance[J].Ichnos,1996.1-17.

6 BuatoisLA,Mangano M G,Xiaotao Wu. Sedimentary facies, depositional process and climatic controls in a Triassic Lake, Tanzhuang Formation, western HenanProvince, China[J].Journal of Paleolimnology,1994.41-46.

7 GorePJW. Paleoecology and sedimentology of a Late Triassic lake, Culpeper Basin, Virginia, USA[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1988.593-608.

8 PlattNH,Wright V P. Lacustrine carbonates: facies models, facies distributions and hydrocarbon aspects[A].IAS Special Publication,1991.57-74.

9 SeilacherA. Events and their signatures An overview[A].Berlin:Springer-Verlag,1991.222-227.

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13 KleinGD. Estimating water depths from analysis of barrier island and deltaic sedimentary sequences[J].Geology,1974.409-412.

14 CohenAS.Tectono-stratigraphic model for sedimentation in Lake Tanganyka, Africa[A].Case studies and modern analogues: AAPG Memoir,1990.137-150.

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17 CurranHA,Frey R W. Pleistocene trace fossils from North Carolina (USA) and their Holocene analogues[A].Liverpool Geological Society,1977.139-162.

18 StanleyKO,Fagerstrom J A. Moicene invertebrate trace fossils from a braided river environment, western Nebraska, USA[J].Palaeogeography Palaeoclimatology Palaeoecology,1974.63-82.

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21 胡斌,吴贤涛,潘丽敏. 川西峨眉晚古生代和中生代河流沉积中的遗迹化石群落[J].沉积学报,1991,(04):128-135.

22 胡斌,吴贤涛. 川西峨眉早白垩世夹关期河流沉积中的遗迹化石群落[J].古生物学报,1993,(04):478-489.

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25 张国成,郭卫星,曾玉凤. 河南西峡盆地晚白垩世河流相-湖泊相沉积中的遗迹组构[J].古地理学报,2004,(04):434-441.

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27 王鸿祯. 中国古地理文集[M].北京:测绘出版社,1985.1-283.

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济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征

1. 河南理工大学,河南焦作 454100;

2. Facultad de Ciencias Naturales Universidad Nacional de Tucum an Casilla de Correo 1 (CC) 4000 San Miguel

基金项目: 国家自然科学基金项目(批准号: 40172045);河南省教育厅基金项目(2003170054);焦作工学院博士基金项目(1005921)资助.

作者简介:
张国成，男，1964年出生，副教授，博士，沉积大地构造学与遗迹学。

收稿日期: 2004-04-15
修回日期: 2004-07-12
刊出日期: 2005-03-10

中图分类号: P512.2;Q911

关键词:

摘要: 济源市西南郊出露有中—上三叠统谭庄组,代表了济源中生代盆地充填的一部分。在湖相剖面中识别出六种岩相组成的两类相序,相序 1呈叠置的向上变粗的序列,由下到上由富有机质页岩 (相E,类型Ⅰ ),纹层粉砂岩 (相A)和水流波痕层理砂岩(相B)组成,记录了在温暖潮湿条件下常年性开放湖泊中小型河口坝三角洲的进积作用;相序 2缺少明显的垂直序列,由互层状细粒碳酸盐岩和粉砂岩(相C),变形层理和波浪改造砂岩 (相D),富有机质页岩(相E,类型Ⅱ)和粘土岩组成,虽然也代表了常年性开放浅水湖泊体系,但反映出很强的季节性气候控制特征。湖相剖面的相C中发育丰富的Skolithos linearis组合,也反映出底层受季节性气候控制。文章深入探讨了该组上段浅湖沉积的环境演替及气候对沉积作用的控制作用,在湖泊演化过程中,很可能出现过几次水体分层。根据晚三叠世时期的古地理重建,推测谭庄组上段湖相沉积反映出的强烈季节性可以用潘加亚巨型季风影响的设想模式解释。

English Abstract

Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation ( T_2-3 ), Jiyuan Basin, Henan Province

1. Henan Polytechnic University,Jiaozuo Henan 454100;

2. Facultad de Ciencias Naturales Universidad Nacional de Tucuman,Casilla de Correo 1 (CC) 4000 San Miguel

Received Date: 2004-04-15
Rev Recd Date: 2004-07-12
Publish Date: 2005-03-10

Keywords:

Abstract: The Middle to Upper Triassic Tanzhuang Form ation, being well cropped out near Jiyuan City, Henan Province,represents a part of the infill of the earlyMesozoic Jiyuan-Yima Basin. The upper part of this stratigraphic unit records deposition with in prevailing shallow lake conditions. S ix sedim entary facies clustered into two facies assemb lages were recognized in the lacustrine section. Facies assemb lage 1 consists of the stacked coarsening-upward sequences composed, from base to top, of organic-rich shale ( facies E, typeⅠ), laminated siltstones (facies A) and current-rippled laminated sandstones (facies B). Units of assemb lages 1 record progradat ion o f smallmouth-bar de ltas with in a perennial open lacustr ine system under temperate and humid cond itions. Facies assemb lage 2 lacks a clear vertical prograd ition pattern and consists of in terbedded f ine-grained carbonates and siltstones ( facies C ); de formed and wave-rewo rked sandstones ( fac ies D ) ; organic-rich shales ( facies E, type Ⅱ ) and clayey mudstones ( facies F). The assemb lage also represents a perennia,l hydro log ica lly open, shallow lacustrine system, but characterized by strong seasona l climatic control. The Skolithos linearismonospecific assemb lagema in ly occurred abundantly in faciesC suggests the substrates contro lled by seasona l climate. Water strat ification probably occurred in severa l periods of the lake history. Pangaean megamonsoonal influence is env isaged to expla in the strong seasonality imprint evidenced tow ard the upper part of the Tanzhuang lacustrine co lumn.

张国成, 曾玉凤, Buatois LA, Mangano MG. 济源盆地谭庄组(T2-3)上段湖相沉积及遗迹化石特征[J]. 沉积学报, 2005, 23(1): 99-107.

引用本文:

张国成, 曾玉凤, Buatois LA, Mangano MG. 济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征[J]. 沉积学报, 2005, 23(1): 99-107.

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济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征

作者简介:
张国成，男，1964年出生，副教授，博士，沉积大地构造学与遗迹学。

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Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation ( T_2-3 ), Jiyuan Basin, Henan Province

计量

目录

济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征

1. 河南理工大学,河南焦作 454100;

2. Facultad de Ciencias Naturales Universidad Nacional de Tucum an Casilla de Correo 1 (CC) 4000 San Miguel

作者简介:
张国成，男，1964年出生，副教授，博士，沉积大地构造学与遗迹学。

English Abstract

Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation ( T_2-3 ), Jiyuan Basin, Henan Province

1. Henan Polytechnic University,Jiaozuo Henan 454100;

2. Facultad de Ciencias Naturales Universidad Nacional de Tucuman,Casilla de Correo 1 (CC) 4000 San Miguel

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济源盆地谭庄组(T2-3)上段湖相沉积及遗迹化石特征

作者简介: 张国成，男，1964年出生，副教授，博士，沉积大地构造学与遗迹学。

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Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation ( T2-3 ), Jiyuan Basin, Henan Province

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出版历程

目录

济源盆地谭庄组(T2-3)上段湖相沉积及遗迹化石特征

1. 河南理工大学,河南焦作 454100; 2. Facultad de Ciencias Naturales Universidad Nacional de Tucum an Casilla de Correo 1 (CC) 4000 San Miguel

作者简介: 张国成，男，1964年出生，副教授，博士，沉积大地构造学与遗迹学。

English Abstract

Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation ( T2-3 ), Jiyuan Basin, Henan Province

1. Henan Polytechnic University,Jiaozuo Henan 454100; 2. Facultad de Ciencias Naturales Universidad Nacional de Tucuman,Casilla de Correo 1 (CC) 4000 San Miguel

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济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征

作者简介:
张国成，男，1964年出生，副教授，博士，沉积大地构造学与遗迹学。

Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation ( T_2-3 ), Jiyuan Basin, Henan Province

济源盆地谭庄组(T_2-3)上段湖相沉积及遗迹化石特征

1. 河南理工大学,河南焦作 454100;

2. Facultad de Ciencias Naturales Universidad Nacional de Tucum an Casilla de Correo 1 (CC) 4000 San Miguel

作者简介:
张国成，男，1964年出生，副教授，博士，沉积大地构造学与遗迹学。

Lacustrine Deposits and Associated Trace Fossils in the Upper Part of the Tanzhuang Formation ( T_2-3 ), Jiyuan Basin, Henan Province

1. Henan Polytechnic University,Jiaozuo Henan 454100;

2. Facultad de Ciencias Naturales Universidad Nacional de Tucuman,Casilla de Correo 1 (CC) 4000 San Miguel