| 贵州贵阳贞丰地区早中三叠世深水碳酸盐斜坡沉积特征、演化和构造控制 |
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| 引用本文： | 秦建华,颜仰基.贵州贵阳贞丰地区早中三叠世深水碳酸盐斜坡沉积特征、演化和构造控制[J].沉积学报,1999,17(4):547-552. |
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| 作者姓名： | 秦建华 颜仰基 |
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| 作者单位： | 地矿部成都地质矿产研究所 成都 610082 |
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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。
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| 关 键 词： | 贵州贵阳贞丰 早中三叠世 碳酸盐斜坡 构造控制 |
| 收稿时间： | 1998-03-04 |
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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| QIN Jian,hua,YAN Yang,ji,WU Yin,ling,TAN Qin,yin.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[J].Acta Sedimentologica Sinica,1999,17(4):547-552. |
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| Authors: | QIN Jian hua YAN Yang ji WU Yin ling TAN Qin yin |
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| Institution: | Chengdu Institute of Geology and Mineral Resources,Chengdu 610082,PRC |
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| 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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| Keywords: | Guiyang and Zhengfeng area Early Middle Triassic carbonate slope tectonic control |
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