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JOURNAL OF MECHANICAL ENGINEERING  > 2020  >  38(4): 747-758.
MoZhen GUO, FuLiang LÜ, FuDou Hou, Lin LI, TaoTao YANG, Dong LI. Microbial Composition and Significance of Lower Pliocene Sedimentary Globigerinid Limestone Facies in the East Java Basin[J]. JOURNAL OF MECHANICAL ENGINEERING, 2020, 38(4): 747-758. doi: 10.14027/j.issn.1000-0550.2019.070
Citation: MoZhen GUO, FuLiang LÜ, FuDou Hou, Lin LI, TaoTao YANG, Dong LI. Microbial Composition and Significance of Lower Pliocene Sedimentary Globigerinid Limestone Facies in the East Java Basin[J]. JOURNAL OF MECHANICAL ENGINEERING, 2020, 38(4): 747-758. doi: 10.14027/j.issn.1000-0550.2019.070
shu

Microbial Composition and Significance of Lower Pliocene Sedimentary Globigerinid Limestone Facies in the East Java Basin

doi: 10.14027/j.issn.1000-0550.2019.070
Funds:

Scientific Research and Technological Development Program of China National Petroleum Corporation 2019⁃D4309

  • Received Date: 29 Apr 2019
  • Publish Date: 10 Aug 2020
    Abstract
  • Globigerinid limestone is well developed in the Pliocene Series of the East Java Sea Basin, and has become one of the main exploration targets in this area. Many oil and gas fields have been discovered in Globigerinid limestone reservoirs. Globigerinid limestone is dominated by Foraminifera tests, particularly of the planktonic genus Globiegerina, which may form up to 50 percent of the limestone. Pore space in the limestone comprises foraminiferal test pores and intergranular pores. The porosity of the grainstones may exceed 50 percent, which represents a high⁃quality reservoir. Due to the lack of reliable facies markers, however, opinions differ as to its origin and depositional environment, seriously affecting knowledge of the control factors and distribution of such reservoirs, and limiting exploration in the area.This study examined the depositional environment of Globigerinid limestone based on thin sections of casts, core observations and microbial data, together with the ecological environment of planktonic Foraminifera. It is concluded that the Globigerinid limestone consists of different species, including shallow⁃water species, middle⁃water species and deep⁃water species, as well as tropical⁃, subtropical⁃ and temperate⁃water species. Globigerina bulloides and Globorotalia menardii were found in large quantities, indicating the existence of upwelling. The combined characteristics of the paleosedimentary environment and paleocurrents indicate that the formation of Globigerinid limestone in the study area was closely related to upwelling, and occurred in two stages: firstly, the planktonic foraminiferal species living in the shelf slope and middle ocean were deposited on the sea bed after their death. The bottom current and upwelling current carried the different species to the shelf margin where the energy is weakest and they accumulated there, influenced by offshore currents. Secondly, they were winnowed and transported by waves or storm⁃associated currents, eventually forming one of the primary high⁃quality reservoir exploration targets in the East Java Bain.

     

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