[1]蔡雄飛,羅中杰,葉 琴.湖南四都坪南沱組沉積特征與古氣候變化耦合關系[J].華東地質,2017,38(02):91-98.[doi:10.16788/j.hddz.32-1865/P.2017.02.002]
 CAI Xiong-fei,LUO Zhong-jie,YE Qin.Sedimentary characteristics of the Nantuo Formation in Siduping, Hunan and its coupling relationship with paleoclimate[J].East China Geology,2017,38(02):91-98.[doi:10.16788/j.hddz.32-1865/P.2017.02.002]
點擊復制

湖南四都坪南沱組沉積特征與古氣候變化耦合關系()
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《華東地質》[ISSN:2096-1871/CN:32-1865/P]

卷:
38
期數:
2017年02期
頁碼:
91-98
欄目:
基礎地質
出版日期:
2017-06-15

文章信息/Info

Title:
Sedimentary characteristics of the Nantuo Formation in Siduping, Hunan and its coupling relationship with paleoclimate
文章編號:
2096-1871(2017)02-091-08
作者:
蔡雄飛羅中杰葉 琴
(中國地質大學生物地質與環境地質國家重點實驗室,武漢 430074; 中國地質大學地球科學學院,武漢 430074)
Author(s):
CAI Xiong-feiLUO Zhong-jieYE Qin
(State Key Laboratory of Biogeology and Environmental Geology,Wuhan 430074,China; School of Earth Sciences, China University of Geosciences, Wuhan 430074,China)
關鍵詞:
冰磧巖 沉積特征 古氣候 南沱組 湖南
Keywords:
tillite sedimentary characteristics paleoclimate Nantuo Formation Hunan Province
分類號:
P588.2
DOI:
10.16788/j.hddz.32-1865/P.2017.02.002
文獻標志碼:
A
摘要:
運用現代冰川理論并結合南沱組冰磧巖研究現狀,根據湖南四都坪南沱組宏觀地層序列和微觀構造特征,識別并總結2期冰期和2期間冰期沉積特點,認為冰磧巖前緣是沉積作用活躍地帶,以重力碎屑流、濁流為特點,間冰期以深水和淺水的牽引流為特點。結合沉積作用與古氣候、海平面變化特征,認為該區南沱組冰磧巖由古氣候控制,海平面的起落導致形成不同的沉積類型。
Abstract:
On the basis of the modern theory of glacier and research progress of the Nantuo Formation tillite, this study summarized the sedimentary features of the two glacial periods and two interglacial periods in combination to the macroscopic stragtigraphic sequences and microscopic structures of the Nantuo Formation in Siduping of Hunan Province. The results show that the front margin of the tillite is an active zone of sedimentation characterized by gravitational debris flow and turbidity current. And the interglacial period was characteristic of deep and shallow water tractive current deposits. The sedimentation of the Nantuo Formation and change characteristic of paleoclimate and sea level suggest that the tillite of the Nantuo Formation was controlled by the paleoclimate and the big fluctuations of sea level resulted in various sedimentary types.

參考文獻/References:

[1] 張啟銳,儲雪蕾.揚子地區江口冰期地層的劃分對比與南華系層型剖面[J].地層學雜志,2006,30(4):306-314.

[2] 張啟銳,儲雪蕾,馮連君. 關于華南板塊新元古代冰川作用及其古緯度的討論[J].科學通報,2009, 54(7): 978-980.
[3] Willis B,Blackwelder E,Sargent H, etal. Stratigraphy of Shan-Tung[J].Research in China,1907,1(1):19-58.
[4] Grabau A W. The Sinian System [J].Acta Geological Sinica, 1922,1(1/4):44-88.
[5] 張啟銳.湖北省宜昌縣震旦系南沱組成因的新認識[J].地質科學,1995,30(2):147-152.
[6] 趙自強,邢裕盛,馬國干,等. 湖北峽東震旦系[M]. 天津:科學技術出版社,1980:31-55.
[7] 馬國干,王硯耕.鄂、湘、川、黔毗鄰地區早震旦世冰川地質問題的討論[J].中國地質科學院宜昌研究所所刊,1983(7):43-52.
[8] 陸松年,馬國干,高振家,等.中國晚前寒武紀冰成巖系初探[M]. 北京:地質出版社,1985:1-86.
[9] 瞿樂生,余林青,吳斯江,等. 湖北省各時代巖相古地理研究之一:溯北省震旦紀巖相古地理[M].武漢:中國地質大學出版社,1990:89.
[10] 劉鴻允.中國震旦系[M].北京:科學出版社,1991:1-388.
[11] 李銓,冷堅. 神農架上前寒武系[M].天津:科學技術出版社,1987:274-335.
[12] 湖南地質礦產局. 湖南巖石地層[M].武漢:中國地質大學出版社,1997:50-51.
[13] 劉波.大庸市四都坪震旦系南沱組巖石特征及成因探討[J].湖南地質,1990,9(4):43-50.
[14] 王劍.華南新元古代裂谷盆地沉積演化——兼論與Rodinia解體的關系[D].成都:成都理工大學,1999:1-146.
[15] 馮連君,儲雪蕾,張啟銳,等.化學蝕變指數(CIA)及其在新元古代碎屑巖中的應用[J].地學前緣,2003,10(4):539-543.
[16] 馮連君,儲雪蕾,張啟銳,等.湘西北南華系渫水河組寒冷氣候成因的新證據[J].科學通報,2004,49(12):1171-1178.
[17] 王自強,尹崇玉,高林志,等.宜昌三斗坪地區南華系化學蝕變指數特征及南華系劃分、對比的討論[J].地質論評,2006, 52(5):577-585.
[18] 趙小明,劉圣德,張權緒,等.鄂西長陽南華系地球化學特征的氣候指示意義及地層對比[J].地質學報,2011,85(4):576-585.
[19] 劉波. 華南震旦系冰川地層及冰川演化規律[J].成都理工大學學報(自然科學版),1991,18(2):40-47.
[20] Crossman M J. Large floods and climatic change during the Holocene on the Ara River, Central Japan[J].Geomorphology,2001,39(1/2):21-27.
[21] 洪慶玉. 沉積物重力流地質學[M].成都:成都科技大學出版社,1987:22-26.
[22] 蔡雄飛,廖群安,王富明,等.新疆卡拉麥里碰撞帶南緣志留—泥盆紀沉積學研究新進展[J].華東地質,2016,37(2):113-119.
[23] 吳瑞棠,關保德. 論羅圈組的冰成特征及重力流改造[J].地質學報,1988,62(1):78-89.
[24] Gravenor C P, Brunn V V, Dreimanis A. Nature and classification of waterlain glaciogenic sediments, exemplified by Pleistocene, Late Paleozoic and Late Precambrian deposits[J]. Earth Science Reviews, 1984, 20(2):105-166.
[25] Kurtz D D, Anderson J B. Recognition and sedimentologic description(texture)of recent debris flow deposits from the Ross and weddell Seas, Antarctica[J]. Journal of Sedimentary Petrology,1979,49(4):1159-1169.
[26] Suttner L J, Dutta P K. Alluvial sandstone composition and paleoclimate; I,Framework mineralogy[J].Journal of Sedimentary Research,1986,56(3):329-435.

相似文獻/References:

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 CAI Xiong-fei,LUO Zhong-jie.Sedimentary features of the Doushantuo Formation in Siduping, northwestern Hunan Province and their paleogeographical significance[J].East China Geology,2018,39(02):11.[doi:10.16788/j.hddz.32-1865/p.2018.01.002]

備注/Memo

備注/Memo:
*收稿日期:2016-06-24 修訂日期:2016-08-18 責任編輯:譚桂麗
基金項目:中國地質調查局“神農架―雪峰山地區區域地質專項調查(項目編號:12120114066301)”資助。
第一作者簡介:蔡雄飛,1952年生,男,研究員,主要從事地層學和沉積學研究。
更新日期/Last Update: 2017-06-16
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