| 滇中梅树村剖面筇竹寺组等深流沉积的发现及其意义 |
| |
| 引用本文： | 李向东,陈海燕.滇中梅树村剖面筇竹寺组等深流沉积的发现及其意义[J].高校地质学报,2019,25(3):412. |
| |
| 作者姓名： | 李向东 陈海燕 |
| |
| 作者单位： | 昆明理工大学国土资源工程学院,昆明,650093;昆明理工大学国土资源工程学院,昆明,650093 |
| |
| 基金项目： | 云南省教育厅科研项目;国家自然科学基金;昆明理工大学自然科学研究项目 |
| |
| 摘 要： | 寒武系筇竹寺组是中国南方页岩气勘探的重要目标层位之一，同时也是澄江动物群的寄主层位，但对其沉积环境和
沉积作用的研究相对薄弱。文章以滇中地区昆阳梅树村剖面为研究对象，在详细的野外观察基础上，应用指向沉积构造进
行了古水流分析，并对广泛发育的条纹、条带构造进行了详细研究。结果表明：（1） 交错层理与小型槽模所表示的古水流
夹角在43°和108°之间，集中分布的区间为50°和79°之间，其中同一薄层粉砂岩中两者的夹角平均值为50°，大于45°；
（2） 条纹、条带构造在垂向上多数显示出双向递变的周期性特征，其中有的条纹构造还表现为多个周期的复合。结合当时
的古地理特征和筇竹寺组的深水沉积环境，可推断沉积流体流动方向与古区域斜坡倾向存在大角度夹角，并且水流具有明
显周期性特征，故可能为深水等深流。筇竹寺组深水等深流沉积的发现对于中国南方筇竹寺组页岩气烃源岩和储集层的分
布研究以及澄江动物群的生存条件、死亡因素和软体化石的保存条件的研究均具有重要意义。
|
| 关 键 词： | 等深流沉积 条纹、条带构造 古水流分析 筇竹寺组 |
Discovery of Contourite and Its Significance in Qiongzhusi Formation of Meishucun Section,Central Yunnan Province,China |
| |
| LI Xiangdong,CHENHaiyan.Discovery of Contourite and Its Significance in Qiongzhusi Formation of Meishucun Section,Central Yunnan Province,China[J].Geological Journal of China Universities,2019,25(3):412. |
| |
| Authors: | LI Xiangdong CHENHaiyan |
| |
| Abstract: | Although Qiongzhusi Formation of Cambrian is one of the most important shale gas exploration targets in South China and
the host rock of Chengjiang Fauna, studies of its sedimentary environments and processes are still inadequate. This study is focused on
the Meishucun Section of Kunyang in central Yunnan Province, where palaeocurrents with directional sedimentary structures are
analyzed and the extensive stripped-and-banded structures in Qiongzhusi Formation are studied based on detailed field observations.
The results show that (1) the palaeocurrent angles between cross-beddings and small flutes are from 43°to 108°, with distribution
mainly between 50° and 79°, and the average angle in the same thin-bedded siltstone is 50°, greater than 45°; (2) most stripped and
banded sedimentary structures have a bidirectional periodic evolution in vertical and some of stripped structures behave a compound of
multiple periods. According to the palaeogeography and the deep-water deposition environment of Qiongzhusi Formation, we suggest
that the deep-water contour currents are responsible for these deposits because of the large angle between the flow direction of
sedimentary currents and the dip azimuth of the ancient regional slope, and also an obvious period of the depositional currents. The
discovery of deep-water contourites in Qiongzhusi Formation has an important significance for understanding the distribution of shale
gas source rocks and reservoir of Qiongzhusi Formation in South China, as well as the survival conditions, death factors and
conservation conditions of the mollusks fossil in Chengjiang fauna. |
| |
| Keywords: | contourite stripped-and-banded structure palaeocurrent analysis Qiongzhusi Formation |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
| 点击此处可从《高校地质学报》浏览原始摘要信息 |
|
点击此处可从《高校地质学报》下载全文 |
|
