| 陆相层序地层学进展 |
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| 引用本文： | 程日辉,王东坡.陆相层序地层学进展[J].沉积与特提斯地质,1996,16(4):56-61. |
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| 作者姓名： | 程日辉 王东坡 |
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| 作者单位： | 长春地质学院 |
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| 摘 要： | 陆相层序地层学是层序地层学发展的一个重要方向．由于陆相地层的特点，其与海相层序地层相比具有特殊性。本文从层序的控制因素、层序界面、基准面、体系域与沉积体系的发育、层序地层与模拟技术和全球对比意义等方面回顾了陆相层序地层学的进展并讨论了陆相层序地层学的特点。
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| 关 键 词： | 陆相层序地层学，控制因素，层序界面，体系域，全球对比 |
| 收稿时间： | 1995/5/15 0:00:00 |
DEVELOPMENTS IN SEQUENCE STRATIGRAPHY OF CONTINENTAL STRATA |
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| Cheng Rihui,Wang Dongpo.DEVELOPMENTS IN SEQUENCE STRATIGRAPHY OF CONTINENTAL STRATA[J].Sedimentary Geology and Tethyan Geology,1996,16(4):56-61. |
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| Authors: | Cheng Rihui Wang Dongpo |
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| Institution: | Changchun Universal of Earth Sciences |
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| Abstract: | Sequence stratigraphy of continental strata which are greatly different from those ofmarine strata is an important branch in the field of sequence stratigraphy. The developments are reviewed on the basis of contrOlling factors of sedimentary systems,sequence stratigraphy and simulation,and global correlation,and characteristics of seuqence stratigraphy'of continental strata are also illustrated in this paper. |
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| Keywords: | sequence stratigraphy of continental strata controlling factor sequenceboundary systems tract global correlation |
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