Quantitative reconstruction of Middle and Late Eocene paleoclimate based on palynological records from the Huadian Basin, northeastern China: Evidence for monsoonal influence on oil shale formation

2018 ◽  
Vol 510 ◽  
pp. 63-77 ◽  
Author(s):  
Qing-tao Meng ◽  
Angela A. Bruch ◽  
Ge Sun ◽  
Zhao-jun Liu ◽  
Fei Hu ◽  
...  
1994 ◽  
Vol 21 (1) ◽  
pp. 67-89 ◽  
Author(s):  
Joseph A. Curiale ◽  
Martin R. Gibling
Keyword(s):  

2009 ◽  
Vol 49 (6) ◽  
pp. 454-457 ◽  
Author(s):  
R. S. Min ◽  
T. A. Sagachenko ◽  
V. A. Kashirtsev ◽  
O. N. Chalaya ◽  
A. Yu. Kuchkina

2016 ◽  
Vol 12 (2) ◽  
pp. 255-272 ◽  
Author(s):  
Y. X. Li ◽  
W. J. Jiao ◽  
Z. H. Liu ◽  
J. H. Jin ◽  
D. H. Wang ◽  
...  

Abstract. The Paleogene sedimentary records from southern China hold important clues to the impacts of the Cenozoic climate changes on low latitudes. However, although there are extensive Paleogene terrestrial archives and some contain abundant fossils in this region, few are accurately dated or have a temporal resolution adequate to decipher climate changes. Here, we present a detailed stratigraphic and paleomagnetic study of a fossiliferous late Paleogene succession in the Maoming Basin, Guangdong Province. The succession consists of oil shale of the Youganwo Formation (Fm) in the lower part and the overlying sandstone-dominated Huangniuling Fm in the upper part. Fossil records indicate that the age of the succession possibly spans the late Eocene to the Oligocene. Both the Youganwo Fm and the overlying Huangniuling Fm exhibit striking sedimentary rhythms, and spectral analysis of the depth series of magnetic susceptibility of the Youganwo Fm reveals dominant sedimentary cycles at orbital frequency bands. The transition from the Youganwo oil shale to the overlying Huangniuling sandstones is conformable and represents a major depositional environmental change from a lacustrine to a deltaic environment. Integrating the magnetostratigraphic, lithologic, and fossil data allows establishing a substantially refined chronostratigraphic framework that places the major depositional environmental change at 33.88 Ma, coinciding with the Eocene–Oligocene climate transition (EOT) at  ∼ 33.7 to  ∼ 33.9 Ma. We suggest that the transition from a lacustrine to deltaic environment in the Maoming Basin represents terrestrial responses to the EOT and indicates prevailing drying conditions in low-latitude regions during the global cooling at EOT.


2021 ◽  
Vol 39 (2) ◽  
pp. 417-423
Author(s):  
Pengfei Jiang ◽  
Danlei Zhang ◽  
Bin Li ◽  
Chao Song

An in-situ pyrolysis technology was proposed for shallow oil shale: drilling horizontal wells to the oil shale formation, connecting the horizontal well sections through hydraulic fracturing, injecting nitrogen from the surface to bottomhole, heating up the nitrogen to a high temperature at the bottom, and directly using the high-temperature nitrogen for oil shale pyrolysis. Then, a mathematical model was established for the heat transfer within the oil shale, and a simplified physical model was created for in-situ pyrolysis of oil shale, and used to simulate the heat transfer process. The simulation results show that, with the extension of heating time, the area of effectively pyrolyzed oil shale formation took up an increasingly large proportion of the total cross-sectional area of the formation; however, the increase of the pyrolysis area ratio was rather slow, and the temperature was unevenly distributed in the formation after a long duration of heating. Therefore, the 300d in-situ heating was split into two stages: 250d of heating in the heating well and 50d of heating in the production well. The two-stage heating maximized the heating area of oil shale, and heated 57% of the cross-sectional area up to 400℃, ensuring the effectiveness of pyrolysis. Moreover, this heating scheme ensured an even distribution of temperature in oil shale formation, a high energy utilization, and a desirable heating effect.


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