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震积

震积

震积

1

They were formed in a dry tidal flat lagoon environment , and developed in the upper part of the Lower Cambrian .

震积岩形成于干燥的潮坪泻湖环境，发育在下寒武统的上部。

2

Sedimentary facies indicators are the best effective criteria to identify seismites .

震积岩相标志是识别震积岩的最有效依据。

3

Through a comprehensive correlation of the strata , the isochroneity of seiemites in different areas is proved in the paper .

本文通过地层综合对比，论证了不同地区震积岩的等时性。

7

Characteristics and Geological Significance of Seismites of the Yanchang Formation, Upper Triassic, Ordos Basin

鄂尔多斯盆地南部上三叠统延长组震积岩的发现及地质意义

10

Paleozoic Seismites in the Nandan-Hechi Basin, Guangxi and Its Tectonic Significance

广西丹池盆地晚古生代震积岩及其构造意义

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