| 什邡式磷块岩矿床的成矿条件与冲断推覆构造 |
| |
| 引用本文： | 黄富荣,邓小林.什邡式磷块岩矿床的成矿条件与冲断推覆构造[J].化工矿产地质,2011,33(1):27-32,36. |
| |
| 作者姓名： | 黄富荣 邓小林 |
| |
| 作者单位： | 中化地质矿山总局地质研究院,河北,涿州,072754 |
| |
| 摘 要： | 什邡式磷矿床产于松潘——甘孜造山带,受同沉积断块的控制,分布在六水闸推覆体周边,磷质来源于清平磷矿层和绵竹磷矿层,沉积环境为滞流海湾,古地貌是水下隆起,并在不断隆升中成矿.成矿后遭受冲断推覆运动的改造,形成大量柔流褶皱和阶梯断层.与沉降带磷块岩矿床地质特征有很大区别.
|
| 关 键 词： | 成矿条件 冲断推覆 磷块岩矿床 |
METALLOGENIC CONDITIONS AND THRUST DECKEN STRUCTURE OF SHIFANG PHOSPHORITE DEPOSITS |
| |
| Huang Furong,Deng Xiaolin.METALLOGENIC CONDITIONS AND THRUST DECKEN STRUCTURE OF SHIFANG PHOSPHORITE DEPOSITS[J].Geology of Chemical Minerals,2011,33(1):27-32,36. |
| |
| Authors: | Huang Furong Deng Xiaolin |
| |
| Institution: | Huang Furong Deng Xiaolin Geological Institute of China Chemical Geology and Mine Bureau,Zhuozhou,Hebei,072754,China |
| |
| Abstract: | Be controlled by sedimentary fault block and distributed around Liushuizha nappe,Shifang phosphorite deposits occur in the Songpan-Ganzi orogenic belt,with submarine upheaval,they sedimented in stagnant gulf.The phosphatic materials origined from Qingping and Miaozhu phosphorite ledge and formed a great deal of flow foldings and terrace faults after suffering nappe reformation,all of which are different from the characters of phosphorite deposit in depression area. |
| |
| Keywords: | metallogenic conditions thrust nappe phosphorite deposit |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
