The Sedimentary Characteristic and Evolution of the Early Middle Triassic Deep Water Carbonate Slope in Guiyang and Zhengfeng Area,Guizhou Province and Its Tectonic Controls
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摘要: 早中三叠世贵州贵阳贞丰地区构造上位于南盘江盆地西北缘,其深水碳酸盐斜坡沉积作用由原地碳酸盐和异地碳酸盐组成。其中,异地碳酸盐有碎屑流、变密度颗粒流、浊流和沉积物滑动4种类型。组成了碳酸盐同斜缓坡、沉积型斜坡和跌积型斜坡三种斜坡沉积类型。在早中三叠世全球海平面上升背景下,碳酸盐斜坡沉积主要受构造活动的控制。早三叠世,盆地处于被动边缘,碳酸盐斜坡经历了由缓坡到进积型沉积斜坡的发展。中三叠世随着盆地进入到前陆盆地的演化,碳酸盐斜坡受挠曲引张作用影响,发展成后退的跌积型斜坡,并经历了从阶梯状后退到连续后退的演化。Abstract: The excellent outcrops developped in Guiyang and Zhengfeng area,Guizhou Province in early and middle Triassic.In the context of the tectonic setting,Guiyang and Zhengfen area,Guizhou province,is situated at the northwestern basinal margin of the Nanpanjiang basin in early and middle Triassic.The sedimentary characteristic of the deep water carbonate developed in this area was made up of in situ and allochthonous carbonates.Furthermore,the allochthonous carbonates were divided into four types,i.e.,debris flow,density modified grain flow,turbidity and sedimentary slumping. The in situ carbonate was characteristic of gray dark gray thin bedded micritic limestone with the sparse faecal pellets and bioturbated structures,indicating the background deposits of the deep water carbonates. The debris flow deposit was a primary type among the allochthonous carbonates,and composed of the floating brecciola and brecciola. The turbidity flow deposit primarily possessed the Bouma sequence T bc and T ab,and sparsely the whole sequence of T abced which occurred in the middle Triassic. The sedimentary slumping formed the slumpong rock.It possessed not only the partial features of the brecciola,but also retained the primitive character with little matrix.It primarily occurred in upper part of the Qinai Formation (middle Triassic) as the thin bedded micritic limestone. And the deep water carbonate slopes developped into the three kinds of models including homocline ramp,sedimentary slope and by pass slope.In the context of the eustatic sea level rise in early middle Triassic epoch,the evolution of the carbonate slope was mainly controlled by the tectonic activity.With the passive margin,development of Nanpanjiang basin in early Triassic,the carbonate slope evolved from the ramp into the prograding sedimentary slope.And in the middle Triassic,accompanying with the development of the peripheral foreland basin,the evolution of the carbonate slope was affected with the flexural extension in the basin.As a result,the carbonate slope developed into the by pass slope with the evolution from the stepping to successive retreat.
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Key words:
- Guiyang and Zhengfeng area /
- Early-Middle Triassic /
- carbonate slope /
- tectonic control
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[1] 1 秦建华, 吴应林, 颜仰基, 朱忠 发. 南盘江盆 地海西 —印支 期沉积构造演化 [J]. 地质学报, 1996, 70:99～107
2 吴应林, 朱忠发, 王吉礼等. 上扬子台 地早、中三 叠世岩相 古地理及沉积矿产环境控制 [M]. 重庆:重庆出版社, 1989. 46～122
3 王吉礼, 王泽文. 上扬子台地三叠系飞仙关组的碳 酸盐堡岛[A],岩相古地理文集(1)[C], 北京:地质出版社, 1985. 154～165
4 吴应林, 朱洪发, 朱忠发等. 中国南方三叠纪岩相古地理与成矿作用 [M]. 北京:地质出版社, 1994. 30～97
5 Enos P. Flow regimes in debris flow [J]. Sedimentology, 1977, 24 :133～142
6 Lowe D R. Grain flow and grain flow deposi ts [J]. J. Sed., 1976,46:188～199
7 Fisher R V. Flow transformations in sediment gravity flow s [J]. Ge-ology, 1983, 11:273～274
8 Lash G R. D ensity modified grain flow deposits from an Early Paleo-zoic margin [J]. Journal of Sedim entay Petrology, 1984, 54:557～562
9 Read J F. C arbonate platform faci es models [J]. AA PG Bulletin,1985, 69:1～12
10 Read J F. Carbonate platforms of Passive(Extensional) Con tinentalM argins:Types, Characteristi cs and Evolution [J]. Tectonophysics,1982, 81:195～212
11 Emery D, M yers K J. Sequence stratigraphy [M]. Blackw ell S ci-ence b, 1996. 211～238
12 Haq B U, Hardenbol J, V ai l P R. Chronology of fluctating sea levelssince the T riassic[J]. Science, 1987, 235:1 156～1 166
13 Bradley D C, Kidd W S F. Flexural extention of the upper continen-tal crust in collisional foredeeps[J]. Geological S ociety of Ameri canBulletin, 1991, 103:1 416～1 438 -
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