1) Dabieshan / Tongbaishan
桐柏山变质核杂岩
2) Tongbai Complex
桐柏杂岩
1.
The Nature of the Tongbai Complex and Its Tectonic Implications
桐柏杂岩的性质及构造意义
2.
The Tongbai complex is situated between two Indosinian high-pressure(HP) metamorphic belts in the Tongbai area.
桐柏杂岩位于桐柏地区两条印支期高压变质带之间,长期以来被认为是一个前寒武纪变质杂岩体。
3) Queshan metamorphic core complex
鹊山变质核杂岩
1.
On the basis of the structural study of the Pengjiakuang gold deposit in Rushan County, Shandong Province, it has been proven that the Queshan metamorphic core complex and denudational faults control the metallization, including ore\|forming metal sources and structural conditions of mineralization.
对山东乳山蓬家夼金矿区的控矿构造研究表明 ,鹊山变质核杂岩构造及蓬家夼拆离断层带对蓬家夼金矿化的物质来源、成矿的构造条件和物理化学条件等 ,都具有重要的控制作用。
5) Yunmeng Shan metamorphic core complex
云蒙山变质核杂岩
1.
Tectono-thermal evolution of the detachment fault along the southeastern margin of the Yunmeng Shan metamorphic core complex in the northern part of Beijing.;
京北云蒙山变质核杂岩南东侧剥离断层带的构造热演化
补充资料：桐柏山
| 桐柏山 位于中国河南省、湖北省边境地区。属淮阳山脉西段。西北-东南走向。西起南阳盆地，东止鸡公山，长100余千米。主峰太白顶，海拔1140米，位于山脉最西端桐柏县西。是淮河的发源地。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条