| 郯庐断裂中段古裂谷的基本特征 |
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| THE MAIN CHARACTERISTICS OF THE PALEORIFT IN THE MIDDLE SECTION OF THE TANCHENG--LUJIANC FRACTURE ZONE |
| The evidence of the paleorift (J_3-K_2) in the middle section of the Tan-cheng-Lujiang Fracture Zone is described here in detail. A preliminary conc-lusion about the paleorift is obtained through reconstruction of paleotectonicsand paleogeomorphology, elucidation of magmatic evoluttion and deep struct-ures, and comparison with some typical rifts in the world. |
| XU Zhi-qin,ZHANG Qiao-da,ZHAO Min.1982.THE MAIN CHARACTERISTICS OF THE PALEORIFT IN THE MIDDLE SECTION OF THE TANCHENG--LUJIANC FRACTURE ZONE[J].Acta Geoscientica Sinica,4(1):17-44. |
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