Sill emplacement during rifting and inversion from threedimensional seismic and well data, Phitsanulok Basin, Thailand
The Cenozoic Phitsanulok rift basin (Thailand) is extensively affected by igneous intrusions and lava flows. In the Ruang Thong-Sai Ngam area, the E-A01 well drilled the early Miocene synrift Lan Krabu Formation, and unexpectedly encountered a 300-m-thick olivine dolerite sill (sill 3). The top and...
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| Main Authors: | , , , |
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| 格式: | 雜誌 |
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2018
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| 在線閱讀: | https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85035749332&origin=inward http://cmuir.cmu.ac.th/jspui/handle/6653943832/57199 |
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| 機構: | Chiang Mai University |