2001Acta Petrologica SinicaRequires access

SUMMARY OF THE ABIOGENIC ORIGIN THEORY AND THE ABIOGENIC GAS POOLS(FIELDS)

Jinxing Dai

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Abstract

The research on the abiogenic origin theory in China is in the forward position in the world.Extensive scientific research and practi ce have proven that a relatively large percentage of hydrocarbons,especially oil ,are generated organically.However,this does not rule out the possibility that a nother large proportion of hydrocarbons,gas in particular,may be of abiogenic or igin.The identifications of organic and abiogenic gases are as the follows:1) Th e abiogenic origin CH_4 has a δ~13 C_1 value greater than -30‰; 2) The abiogenic alkane gases have negative carbon isotope sequences; 3) CH_4/ ~3He values are n×10~5~7; 4) Abiogenic δ~13 Cco_ 2 values are greater than -8‰.The Changde Gas Field is possible the first abiog enic hydrocarbon gas field in the world.Favorable locations for abiogenic gas fi elds can be selected by following criteria:1) Existance of Moho up-pouring or m antle plume; 2) High thermal or thermal structural area with a heat flow value g reater than 1.3 HFU and a geothermal gradient higher than 3.5℃/100m; 3) Anomalo us R/Ra1,especially R/Ra2 zones;4) Presence basalt rock zone along the faults near the gas resource.

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What this paper is about

The research on the abiogenic origin theory in China is in the forward position in the world.Extensive scientific research and practi ce have proven that a relatively large percentage of hydrocarbons,especially oil ,are generated organically.However,this does not rule out the possibility that a nother large proportion of hydrocarbons,gas in particular,may be of abiogenic or igin.The identifications of organic and abiogenic gases are as the follows:1) Th e abiogenic origin CH_4 has a δ~13 C_1 value greater than -30‰; 2) The abiogenic alkane gases have negative carbon isotope sequences; 3) CH_4/ ~3He values are n×10~5~7; 4) Abiogenic δ~13 Cco_ 2 values are greater than -8‰.The Changde Gas Field is possible the first abiog enic hydrocarbon gas field in the world.Favorable locations for abiogenic gas fi elds can be selected by following criteria:1) Existance of Moho up-pouring or m antle plume; 2) High thermal or thermal structural area with a heat flow value g reater than 1.3 HFU and a geothermal gradient higher than 3.5℃/100m; 3) Anomalo us R/Ra1,especially R/Ra2 zones;4) Presence basalt rock zone along the faults near the gas resource.

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Available abstract

The research on the abiogenic origin theory in China is in the forward position in the world.Extensive scientific research and practi ce have proven that a relatively large percentage of hydrocarbons,especially oil ,are generated organically.However,this does not rule out the possibility that a nother large proportion of hydrocarbons,gas in particular,may be of abiogenic or igin.The identifications of organic and abiogenic gases are as the follows:1) Th e abiogenic origin CH_4 has a δ~13 C_1 value greater than -30‰; 2) The abiogenic alkane gases have negative carbon isotope sequences; 3) CH_4/ ~3He values are n×10~5~7; 4) Abiogenic δ~13 Cco_ 2 values are greater than -8‰.The Changde Gas Field is possible the first abiog enic hydrocarbon gas field in the world.Favorable locations for abiogenic gas fi elds can be selected by following criteria:1) Existance of Moho up-pouring or m antle plume; 2) High thermal or thermal structural area with a heat flow value g reater than 1.3 HFU and a geothermal gradient higher than 3.5℃/100m; 3) Anomalo us R/Ra1,especially R/Ra2 zones;4) Presence basalt rock zone along the faults near the gas resource.

Key concepts: Abiogenic petroleum origin, Geology, Geochemistry, Methane, Chemistry, Organic chemistry

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