Zobrazeno 1 - 10
of 46
pro vyhledávání: '"Lunju Zheng"'
Publikováno v:
Shiyou shiyan dizhi, Vol 46, Iss 3, Pp 590-600 (2024)
A pyrolysis hydrocarbon generation experiment was conducted on low-maturity marine shale from the Second White Specks (2WS) Formation of the Cretaceous Colorado Group in the Western Canada Basin. Using GC-MS, quantitative analysis of aromatics in nat
Externí odkaz:
https://doaj.org/article/c364714616dc4831aa47ffe3bdddf504
Publikováno v:
Lithosphere, Vol 2024, Iss 1 (2024)
Organic carbon isotopic analysis is a significant approach for oil-source correlation, yet organic carbon isotopic behavior during oil expulsion from saline lacustrine source rocks is not well constrained, and this hinders its wide application for fi
Externí odkaz:
https://doaj.org/article/a861010ca16e4e4693871e34c4f178d8
Publikováno v:
Shiyou shiyan dizhi, Vol 44, Iss 4, Pp 698-704 (2022)
Fluid-rock interaction is critical for the formation of tight sandstone reservoirs, contributing to illustrate the distribution of high-quality reservoirs. In this study, a simulation experiment on the co-evolution of type Ⅲ source rock fluids and
Externí odkaz:
https://doaj.org/article/e12b5d4e52ef424092564dc498748453
Publikováno v:
Shiyou shiyan dizhi, Vol 44, Iss 2, Pp 241-250 (2022)
The Middle Triassic Leikoupo Formation (T2l) has been regarded as one of the most important strata for natural gas exploration in the Western Sichuan Depression of the Sichuan Basin. The main gas source has not been determined due to the controversy
Externí odkaz:
https://doaj.org/article/9ad1a456932d4644b1c98bd4745417ab
Publikováno v:
Shiyou shiyan dizhi, Vol 44, Iss 1, Pp 121-128 (2022)
Chinese marine source rocks are generally at the stage of high- to over-mature, there are still some uncertainties about whether the existing hydrocarbon isotopic indexes can be directly employed to distinguish the genetic types of marine carbonate n
Externí odkaz:
https://doaj.org/article/d31711b751834f8aa38632e4a8654a16
Publikováno v:
Shiyou shiyan dizhi, Vol 43, Iss 5, Pp 862-870 (2021)
Simulation experiment was one of the most valuable methods for the study of hydrocarbon generation, expulsion and retention in source rocks. It was summarized in this paper that the progressing status and development significations of thermal simulat
Externí odkaz:
https://doaj.org/article/85663e512240464e9f33132d560b5c32
Publikováno v:
Lithosphere, Vol 2022, Iss Special 13 (2022)
AbstractPalaeozoic petroleum systems in the South China craton are prospecting frontiers for unconventional oil/gas. Understanding the hydrocarbon generation/retention capacity of source rocks has critical implications for reserve evaluation and targ
Externí odkaz:
https://doaj.org/article/d97fc25ee5994b7d85bae5fc432466c7
Publikováno v:
Shiyou shiyan dizhi, Vol 43, Iss 3, Pp 498-506 (2021)
To understand the effectiveness of hydrocarbon generation, expelling and retention capacities of coaly source rocks, carbonaceous mudstones and mudstones in coal layers and interlayers of different sedimentary environments and ages were selected to c
Externí odkaz:
https://doaj.org/article/b7a730a250084af19b5b4491e929ee7d
Autor:
Zhenkai HUANG, Maowen LI, Lunju ZHENG, Guoliang TAO, Zhiming LI, Qigui JIANG, Menhui QIAN, Tingting CAO, Shuangjian LI, Yujin WO, Dongsheng SUN
Publikováno v:
Shiyou shiyan dizhi, Vol 42, Iss 4, Pp 639-645 (2020)
By comparing the quantitative pore results of geological samples from natural evolution profiles and simulated experiment samples, it is believed that the volume changes of pores of different scales are basically similar throughout the evolution of s
Externí odkaz:
https://doaj.org/article/ce983265af9c4e08ba21a35af1dc8a81
Publikováno v:
Shiyou shiyan dizhi, Vol 42, Iss 3, Pp 428-433 (2020)
The Wufeng-Longmaxi shale in the Sichuan Basin is the only stratum in China to realize commercial development of shale gas. There are some differences in shale gas generation and a lack of direct experimental evidence of the reasons for these differe
Externí odkaz:
https://doaj.org/article/04ed8e8422ae4112b3ea2da6a62a6d64