地洼型外生矿床
大多为形成于地洼盆地中的油气、油页岩、膏盐、铀、铜、铁、煤等沉积矿床，也有形成于地穹隆起上的风化淋滤型矿床、岩溶充填型矿床等。油气主要有块断型、断褶型、潜山型；还有煤田及油页岩等矿床。地洼区的风化淋滤型矿床往往沿断裂带风化淋滤，表现为线型的矿床。较早形成的地洼型外生矿床，若受后来的地洼成矿作用叠加、改造，可变为复式成矿作用形成的多因复成矿床。
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contributed at 2011-10-11
Classification(s)
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Earth System(in Chinese) DIWA structure theory
Detailed Description
| English |
|---|
| Name | exogenic ore deposits of diwa type |
| Chinese |
|---|
| Name | 地洼型外生矿床 |
| Description | 大多为形成于地洼盆地中的油气、油页岩、膏盐、铀、铜、铁、煤等沉积矿床，也有形成于地穹隆起上的风化淋滤型矿床、岩溶充填型矿床等。油气主要有块断型、断褶型、潜山型；还有煤田及油页岩等矿床。地洼区的风化淋滤型矿床往往沿断裂带风化淋滤，表现为线型的矿床。较早形成的地洼型外生矿床，若受后来的地洼成矿作用叠加、改造，可变为复式成矿作用形成的多因复成矿床。 |
How to Cite
NNU_Group (2011). 地洼型外生矿床, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/0ee09441-938f-472f-bc6a-23e140fade11
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