|Table of Contents|

Geochemical Characteristics and Development Mechanism of Upper Paleozoic Dark Mudstone in Huanghua Depression of Bohai Bay Basin, China(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2023年第02期
Page:
306-321
Research Field:
沉积地质与油气勘探
Publishing date:

Info

Title:
Geochemical Characteristics and Development Mechanism of Upper Paleozoic Dark Mudstone in Huanghua Depression of Bohai Bay Basin, China
Author(s):
LI Chuan-ming1; 2;  ZENG Jian-hui1; 2*;  LIU Hai-tao3;  LI Hong-jun4;  LOU Da4;  CUI Yu4;  DONG Xiong-ying4;  LIU Shu-ning1; 2
(1. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China; 2. College of Geosciences, China University of Petroleum, Beijing 102249, China; 3. Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China; 4. Research Institute of Exploration and Development, Dagang Oilfield Company, PetroChina, Tianjin 300280, China)
Keywords:
dark mudstone;  development environment;  formation mechanism;  Upper Paleozoic;  elemental geochemistry;  organic geochemistry;  Huanghua depression
PACS:
P618.13
DOI:
10.19814/j.jese.2022.09044
Abstract:
The dark mudstone of Upper Paleozoic, which is one of the main source rocks in Huanghua depression of Bohai Bay Basin, has important exploration value. In order to further clarify the environment and formation mechanism of organic matter accumulation from the dark mudstone of Upper Paleozoic in Huanghua depression, the petrological, element geochemical and organic geochemical analyses were carried out. The results show that the dark mudstones of Upper Paleozoic in Huanghua depression of Bohai Bay Basin are near source deposits, which are in the transition period from hot and humid to warm and moist climate; the parent rocks are mainly felsic rocks, which are generally in medium to high weathering degree; the sedimentation sorting and recycling are weak, so the source information is well preserved; the enrichment of organic matter of the dark mudstone of Upper Paleozoic in Huanghua depression from the sedimentary period of Taiyuan Formation to the sedimentary period of Lower Shihezi Formation is not controlled by a single factor, but is the result of the joint control and mutual coupling of many factors, such as oxidation-reduction conditions, paleo-productivity, paleo-climate, and sedimentation rate; during the sedimentary period of Taiyuan Formation, the surface water has higher productivity and a relatively reductive sulfurizing underwater environment, which is conducive to the enrichment and preservation of organic matter; during the sedimentation period of Shanxi Formation, the surface water body also maintains high primary productivity under hot and humid conditions, and the higher sedimentation rate is conducive to the preservation of organic matter; during the sedimentary period of Lower Shihezi Formation, the warm and humid climate is conducive to the enrichment of organic matter, but the low deposition rate results in the dilution of organic matter by clay minerals and other inorganic minerals, which is relatively difficult to be preserved.

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Last Update: 2023-05-20