Evidence map›Paper›PMID 37663475›Full record

ArticleACS omega2023

Characteristics of Chaotic Weak Reflection in Carbonate Fracture-Cavity Reservoirs: A Case Study of Ordovician Reservoirs in Block 10 of the Tahe Oilfield, Tarim Basin, China.

Zhipeng Sun, Ruizhao Yang, Penghui Yang, Shijie Zhang, Yuhao Li, Simin Zhao, Feng Geng

Abstract read
In one paragraph

Article in ACS omega, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

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Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

1 citing paper in PubMed.

  1. Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

7 authors.

Zhipeng SunCollege of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, China.ORCID https://orcid.org/0000-0002-7892-0849
Ruizhao YangCollege of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, China.ORCID https://orcid.org/0000-0003-3200-9280
Penghui YangCollege of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, China.
Shijie ZhangCollege of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, China.
Yuhao LiCollege of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, China.
Simin ZhaoCollege of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, China.
Feng GengCollege of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, China.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The identification of carbonate reservoirs is a critical task in oil and gas exploration. Chaotic weak reflection is an important type of reflection characteristic in carbonate reservoirs. Widespread distribution of chaotic weak reflection has been observed in the Ordovician Yijianfang Formation in the Tahe area. However, there is still a lack of systematic research on the distribution, characteristics, reservoir space, and reservoir types of chaotic weak reflection in the Tahe area. To address this issue, this study conducted a comprehensive analysis of multiscale data and found that chaotic weak reflections are distributed within 100 ms below the top interface of the Middle Ordovician. Seismic profiles exhibit a "string of pearls" with a "tail" or "pearl-like" widening feature. On well logs, all three porosity curves exhibit localized peaks, with increases in acoustic (AC) and compensated neutron (CNL) and decreases in density (DEN), while the deep and shallow lateral resistivity (RD, RS) curves show positive amplitude differences. In the FMI, they are represented by dark sinusoidal curves and dark small patches. Based on these response characteristics, two types of reservoir spaces are identified for chaotic weak reflections: high-angle vertical fractures and caves with heights less than 7 m, which can form independent reservoirs or fracture-cavity complexes. Three types of reservoirs are distinguished: fracture, cavity, and cavity-fracture types.

Identifiers

PMID37663475
PMCPMC10468957

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