Peiqiang Zhao

Peiqiang Zhao

orcid

Research Focus & Metrics

Academic Career Length

12Years (2015-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 September 2017 in Marine and Petroleum Geology
Verified
Journal Article
Closed access
PZPeiqiang Zhao
Peiqiang Zhao
ZWZhenlin Wang
Zhenlin Wang
ZSZhongchun Sun
Zhongchun Sun
JCJianchao Cai
Jianchao Cai
LWLiang Wang
Liang Wang

1 December 2019 in Energy
Verified
Journal Article
Closed access
Jianchao CaiJianchao Cai
Jianchao Cai
Zhien ZhangZhien Zhang
Zhien Zhang
WWWei Wei
Wei Wei
DGDongming Guo
Dongming Guo
SLShuai Li
Shuai Li
PZPeiqiang Zhao
Peiqiang Zhao

1 May 2017 in Marine and Petroleum Geology
Verified
Journal Article
Closed access
PZPeiqiang Zhao
Peiqiang Zhao
HMHuolin Ma
Huolin Ma
VRVamegh Rasouli
Vamegh Rasouli
WLWenhui Liu
Wenhui Liu
Jianchao CaiJianchao Cai
Jianchao Cai
ZHZhenhua Huang
Zhenhua Huang

1 August 2016 in AAPG Bulletin
Verified
Journal Article
Closed access
PDF file
PZPeiqiang Zhao
Peiqiang Zhao
ZMZhiqiang Mao
Zhiqiang Mao
ZHZhenhua Huang
Zhenhua Huang
CZChong Zhang
Chong Zhang
With the booming exploration and development of unconventional hydrocarbon resources in source rocks, the estimation of total organic carbon (TOC) content from well logs has become increasingly important because of the significance of TOC in the formation evaluation of those resources. In this paper, a new log overlay method is developed to estimate the TOC content of source rocks with excess radioactivity, but containing little or no potassium feldspar. Specifically, on the basis of previous results of log responses of source rocks, it is believed that the natural gamma ray (GR) log responses of source rocks in the applicable conditions are predominantly contributed by clay minerals and organic matter. A practical clay indicator is established to reflect the clay content using density and neutron logs. The indicator is effective not only in nonsource rocks that contain oil or water but also in source rocks. Furthermore, a new method was developed by overlaying the properly scaled clay indicator curve on the GR curve. In nonsource rocks, including clay-rich rocks and reservoirs saturated with oil or water, the two curves overlie each other, whereas a separation between the curves occurs in organic-rich source rocks. The separation between the curves was defined and expressed and can be used to calculate the TOC consecutively after careful calibration with core data. This method has been successfully applied to two shale gas plays with high-maturity kerogen in the Sichuan Basin, China. In addition, a source rock with low-maturity kerogen was used to verify the new method for its effectiveness, reliability, and widespread adaptability.

1 January 2020 in Marine and Petroleum Geology
Verified
Journal Article
Closed access
PZPeiqiang Zhao
Peiqiang Zhao
LWLiang Wang
Liang Wang
CXChenhao Xu
Chenhao Xu
JFJinhua Fu
Jinhua Fu
YSYujiang Shi
Yujiang Shi
DXDianshi Xiao
Dianshi Xiao

1 January 2019 in Fuel
Verified
Journal Article
Closed access
PZPeiqiang Zhao
Peiqiang Zhao
Mehdi OstadhassanMehdi Ostadhassan
Mehdi Ostadhassan
BSBo Shen
Bo Shen
WLWenhui Liu
Wenhui Liu
AAArash Abarghani
Arash Abarghani
Jianchao CaiJianchao Cai
Jianchao Cai