| 马坑铁矿火山沉积成因探讨 |
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| GEOLOGICAL CHARACTERISTICS OF THE MAKENG IRON DEPOSIT OF MARINE VOLCANO--SEDIMENTARY ORIGIN |
| The Makeng iron deposit of southwestern Fujian Province is situatedwithin the Yonmei depressional zone upon the Caledonide basement. The ironbearing formation is a group of volcanic series of transgressive character.The volcanic rocks are composed mainly of well-differentiated and alteredintermediate-basic potash rocks and"diabase". The main orebody is stratiform, lying conformably and extending continuously between the upper partof Lindi formation (C_1I) and the lower part of Huanglong formation (C_2h). |
| GE Chao-hua,HAN Fa,ZOU Tian-ren,CHEN De-qian.1981.GEOLOGICAL CHARACTERISTICS OF THE MAKENG IRON DEPOSIT OF MARINE VOLCANO--SEDIMENTARY ORIGIN[J].Acta Geoscientica Sinica,3(1):47-69. |
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