2001Unpublished venueRequires access

Study on sequence stratigraphy in Liubei area, Eastern China oil field

Mu Li

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Abstract

The thesis builds up a sequence stratigraphic network of Sahejie formation and a sequence stratigraphic network of reservoirs by the methods of sequence stratigraphy. We separate Sahejie formation into 3 sequences, the main reservoirs into 6 parasequences and compare the most of well logging base on sequence stratigraphic network. Analysis of sediment development history is made and a model of sequence in the work area is built up. We have also explained why the HST of sequence I is becoming thin torward Baigezhuan faults. That is because of parasequence combining and unconformity.

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The thesis builds up a sequence stratigraphic network of Sahejie formation and a sequence stratigraphic network of reservoirs by the methods of sequence stratigraphy. We separate Sahejie formation into 3 sequences, the main reservoirs into 6 parasequences and compare the most of well logging base on sequence stratigraphic network. Analysis of sediment development history is made and a model of sequence in the work area is built up. We have also explained why the HST of sequence I is becoming thin torward Baigezhuan faults. That is because of parasequence combining and unconformity.

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Available abstract

The thesis builds up a sequence stratigraphic network of Sahejie formation and a sequence stratigraphic network of reservoirs by the methods of sequence stratigraphy. We separate Sahejie formation into 3 sequences, the main reservoirs into 6 parasequences and compare the most of well logging base on sequence stratigraphic network. Analysis of sediment development history is made and a model of sequence in the work area is built up. We have also explained why the HST of sequence I is becoming thin torward Baigezhuan faults. That is because of parasequence combining and unconformity.

Key concepts: Sequence stratigraphy, Sequence (biology), Unconformity, Geology, Stratigraphy, Paleontology, Sediment, Oil field

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