| 鲁西幔枝构造及其控矿特征 |
| |
| 引用本文： | 牛树银,孙爱群,李玉静,王宝德,胡华斌,毛景文,李英平. 鲁西幔枝构造及其控矿特征[J]. 地质学报, 2009, 83(5) |
| |
| 作者姓名： | 牛树银 孙爱群 李玉静 王宝德 胡华斌 毛景文 李英平 |
| |
| 作者单位： | 牛树银,孙爱群,王宝德,胡华斌,NIU Shuyin,SUN Aiqun,WANG Baode,HU Huabin(石家庄经济学院资源学院,石家庄,050031);李玉静,LI Yujing(河北省国土资源厅,石家庄,050051);毛景文,MAO Jingwen(河北省国土资源厅,石家庄,050051;中国地质科学院矿产资源研究所,北京,100037);李英平,LI Yingping(山东省地质调查院,济南,250013) |
| |
| 基金项目： | 国家自然科学基金，中国地质调查局资助项目 |
| |
| 摘 要： | 从区域地层(岩体)中老外新分布,环状、放射状断裂的展布,轴部缓倾拆离滑脱构造的发育,幔源岩浆活动以及区域岩石学、岩石化学、同位素地质学等方面,探讨了鲁西幔枝构造特征.研究认为鲁西地区北西向陡倾韧性剪切带切割了深部华北地幔亚热柱向外拆离的地幔岩,导致其减压释荷形成深熔岩浆,强烈而完整的岩浆演化序列表现出岩浆基性程度由高变低、侵入深度由深变浅、围岩蚀变由强变弱的总体演化趋势.幔枝构造演化对内生成矿作用具有明显的控制作用,并带动围岩一起隆升,形成了典型的鲁西幔枝构造.其顶部发育的拆离掀斜断块,使部分内生矿产被抬升到浅部.
|
| 关 键 词： | 幔枝构造 地幔热柱 构造控矿 成矿作用 鲁西地区 |
Mantle Branch Structure in Western Shandong and Its Ore-Controlling Characteristics |
| |
| NIU Shuyin,SUN Aiqun,LI Yujing,WANG Baode,HU Huabin,MAO Jingwen,LI Yingping. Mantle Branch Structure in Western Shandong and Its Ore-Controlling Characteristics[J]. Acta Geologica Sinica, 2009, 83(5) |
| |
| Authors: | NIU Shuyin SUN Aiqun LI Yujing WANG Baode HU Huabin MAO Jingwen LI Yingping |
| |
| Abstract: | The characteristics of mantle branch structures in western Shandong Province, China are discussed in this study, especially distribution characteristics and ages of the regional strata, the development of ring-like and radial faults, the development of gently inclined detachment-slip structures in the axial part, mantle-source magmatic activities, regional petrology, petrochemistry and isotope geology. The study indicated that the NW sharply plunged ductile shear zone in the region of western Shandong cuts ... |
| |
| Keywords: | mantle branch structure mantle plume tectonic ore-controlling minerogenesis region of western Shandong Province |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
