2000•Acta Petrologica SinicaRequires access

THERMAL EVOLUTION IN TARIM BASIN

Li Cheng

Open publisher page 17 citations

Abstract

Thermal evolution, including Palaeotemperature, palaeoheat-flow and hydrocarbon generation history, is simulated from Sinian to the current by 2-D numerical method based on the tectonic along 11 seismic profiles in Tarim Basin. At several well locations, the simulation results match the measured data well. It is indicated that the thermal evolution from Sinian to the current in Tarim Basin can be divided into four stages. (1 )High heat flow (hot basin)thermal evolution from Sinian to Ordovician; (2)Thermal decline from Silurian to later Paleozoic, being 'hot basin' to 'cool basin' 4 (3) The stable thermal evolution (cool basin) in Mesozoic; (4)Thermal evolution of the lithosphere flexibility in Cenozoic. Furthermore, the hydrocarbon generation histories in the three source rocks in Tarim Basin are simulated, and the prospecting accumulations in favorable areas are analyzed taking account of the tectonic evolution.

About this research paper

What this paper is about

Thermal evolution, including Palaeotemperature, palaeoheat-flow and hydrocarbon generation history, is simulated from Sinian to the current by 2-D numerical method based on the tectonic along 11 seismic profiles in Tarim Basin. At several well locations, the simulation results match the measured data well. It is indicated that the thermal evolution from Sinian to the current in Tarim Basin can be divided into four stages. (1 )High heat flow (hot basin)thermal evolution from Sinian to Ordovician; (2)Thermal decline from Silurian to later Paleozoic, being 'hot basin' to 'cool basin' 4 (3) The stable thermal evolution (cool basin) in Mesozoic; (4)Thermal evolution of the lithosphere flexibility in Cenozoic. Furthermore, the hydrocarbon generation histories in the three source rocks in Tarim Basin are simulated, and the prospecting accumulations in favorable areas are analyzed taking account of the tectonic evolution.

Why it matters

OpenAlex reports 17 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Thermal evolution, including Palaeotemperature, palaeoheat-flow and hydrocarbon generation history, is simulated from Sinian to the current by 2-D numerical method based on the tectonic along 11 seismic profiles in Tarim Basin. At several well locations, the simulation results match the measured data well. It is indicated that the thermal evolution from Sinian to the current in Tarim Basin can be divided into four stages. (1 )High heat flow (hot basin)thermal evolution from Sinian to Ordovician; (2)Thermal decline from Silurian to later Paleozoic, being 'hot basin' to 'cool basin' 4 (3) The stable thermal evolution (cool basin) in Mesozoic; (4)Thermal evolution of the lithosphere flexibility in Cenozoic. Furthermore, the hydrocarbon generation histories in the three source rocks in Tarim Basin are simulated, and the prospecting accumulations in favorable areas are analyzed taking account of the tectonic evolution.

Key concepts: Geology, Structural basin, Ordovician, Paleontology, Paleozoic, Lithosphere, Tectonics, Cenozoic

Related papers

Back to paper searchBrowse research topicsOriginal source
THERMAL EVOLUTION IN TARIM BASIN — Research Paper | ScholarLens