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Tarlong Formation

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Journal Article
Journal: GSA Bulletin
Published: 23 June 2017
GSA Bulletin (2017) 129 (9-10): 1252–1265.
...Jinqiang Tian; Jianzhang Liu; Zengbao Zhang; Fuyun Cong Abstract The Middle Permian Tarlong Formation (P 2 t) source rocks in the Turpan-Hami Basin were studied based on multiple geochemical analyses on outcrop samples from the basin edges to reveal the hydrocarbon-generating potential...
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Figure 11. Outcrop photographs of the Upper Permian <b>Tarlong</b> <b>Formation</b>. (A) ...
Published: 01 February 2002
Figure 11. Outcrop photographs of the Upper Permian Tarlong Formation. (A) Example of outcrop extent and quality in the Tarlong Formation in the western Turpan- Hami basin at Aiweiergou (note person at left-center for scale). (B) Complete cross section of a fluvial channel in the Tarlong Formation
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Representative photos for source rocks of the <b>Tarlong</b> <b>Formation</b> at outcrops...
Published: 23 June 2017
Figure 3. Representative photos for source rocks of the Tarlong Formation at outcrops. (A–B) Aiweiergou. (C–D) Qialekan.
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Van Krevelen diagram of kerogens for source rock samples of the <b>Tarlong</b> For...
Published: 23 June 2017
Figure 6. Van Krevelen diagram of kerogens for source rock samples of the Tarlong Formation from seven outcrops. I, II 1 , II 2 , and III—types of kerogen.
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Variation of vitrinite reflectance ( R  o , %) with  T  max  (maximum pyrol...
Published: 23 June 2017
Figure 7. Variation of vitrinite reflectance ( R o , %) with T max (maximum pyrolysis peak temperature, °C) for source rock samples of the Tarlong Formation from seven outcrops.
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The C 29  20S/(20S+20R) versus C 29  ββ/(αα + ββ) sterane ratios for source...
Published: 23 June 2017
Figure 9. The C 29 20S/(20S+20R) versus C 29 ββ/(αα + ββ) sterane ratios for source rock samples of the Tarlong Formation from seven outcrops. R o —vitrinite reflectance.
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Figure 10. Detailed measured sections of the lower Upper Permian <b>Tarlong</b> Fo...
Published: 01 February 2002
Figure 10. Detailed measured sections of the lower Upper Permian Tarlong Formation (P2t) along the northern Turpan-Hami basin. Sections are presented from west to east (see Fig. 1 for locations and Fig. 3 for legend)
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Variation of Rock-Eval S 1  + S 2  with total organic carbon (TOC) content ...
Published: 23 June 2017
Figure 4. Variation of Rock-Eval S 1 + S 2 with total organic carbon (TOC) content for source rock samples of the Tarlong Formation from seven outcrops. Classifications of source rock quality are from Wang and Chen (1988) . S 1 —soluble hydrocarbon content; S 2 —pyrolysis hydrocarbon content.
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Figure 15. Outcrop photograph of the angular unconformity separating lower ...
Published: 01 February 2002
Figure 15. Outcrop photograph of the angular unconformity separating lower Upper Permian rocks of the Tarlong Formation (P2t) from Triassic strata at Aiweiergou in the western Turpan-Hami basin (see Fig. 1 for location). Stratigraphic relationships indicate that the folding occurred in latest
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Variation of Rock-Eval hydrogen indices with  T  max  for source rock sampl...
Published: 23 June 2017
Figure 5. Variation of Rock-Eval hydrogen indices with T max for source rock samples of the Tarlong Formation from seven outcrops. Classifications of source rock quality are from Tissot and Welte (1984) . TOC—total organic carbon; R o —vitrinite reflectance; HC—hydrocarbon content; T max
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Figure 19. Schematic time series (T 1  through T 4 ) illustrating the Late ...
Published: 01 February 2002
to the geographic northern Tian Shan. See Figure 2 for formation abbreviations. Northern Junggar basin units include the Jiangjunmiao Formation (P2jg) and the Pingdiquan Formation (P2p). (A) Progradation of Daheyen Formation clastic wedge. (B) Interpreted partitioning of the Turpan-Hami basin lake (lower Tarlong
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Representative mass chromatograms of Total Ion Chromatogram (TIC) terpane (...
Published: 23 June 2017
Figure 8. Representative mass chromatograms of Total Ion Chromatogram (TIC) terpane ( m / z = 191) and sterane ( m / z = 217) series of saturated fractions of the Tarlong Formation (P2t) source rock samples from seven outcrops. C 19 –C 26 —C 19 –C 26 tricyclic terpanes; C 24 Tet—C 24
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( on this and following page ). Correlation between various biomarker param...
Published: 23 June 2017
Figure 10 ( on this and following page ). Correlation between various biomarker parameters reflecting organic matter input and/or depositional environments for source rock samples of the Tarlong Formation from seven outcrops. Pr/Ph—pristane/phytane; G/H—gammacerane/αβ C 30 hopane; C 27 /C 27 —C
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( on this and following page ). Correlation between various biomarker param...
Published: 23 June 2017
Figure 10 ( on this and following page ). Correlation between various biomarker parameters reflecting organic matter input and/or depositional environments for source rock samples of the Tarlong Formation from seven outcrops. Pr/Ph—pristane/phytane; G/H—gammacerane/αβ C 30 hopane; C 27 /C 27 —C
Journal Article
Journal: GSA Bulletin
Published: 01 February 2002
GSA Bulletin (2002) 114 (2): 131–152.
...Figure 11. Outcrop photographs of the Upper Permian Tarlong Formation. (A) Example of outcrop extent and quality in the Tarlong Formation in the western Turpan- Hami basin at Aiweiergou (note person at left-center for scale). (B) Complete cross section of a fluvial channel in the Tarlong Formation...
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Series: AAPG Studies in Geology
Published: 01 January 2000
DOI: 10.1306/St46706C8
EISBN: 9781629810713
... ; Carroll et al., 1992 ,1995). (C) Detailed measured section of the upper portion of the lower Upper Permian Tarlong Formation of the Turpan-Hami basin exposed at Zaobishan along the south-central Bogda Shan. (D) Detailed measured section of the lower portion of the Upper Permian Quanzijie Formation...
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Journal Article
Published: 21 May 2021
Geological Magazine (2021) 158 (10): 1847–1861.
... four sections, including the Zhaobishan, North Tarlong, Taodonggou and Dalongkou sections, are the focus of this study (Fig.  2 ). The Bogda Mountains is a giant E–W-directed anticline with Devonian–Quaternary sedimentary and igneous rocks, located between the Junggar Basin to the north and Turpan-Hami...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 2004
AAPG Bulletin (2004) 88 (4): 447–481.
... lacustrine facies of the Turpan-Hami basin to the more basinal facies of the Junggar basin to the north ( Figure 1A ). In Turpan-Hami, the best exposure of organic-rich horizons are in the Tarlong Formation (P2t) in the north-central basin, at Zaobishan ( Figure 4A ). The fine-grained sections...
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Journal Article
Published: 26 April 2019
Journal of Sedimentary Research (2019) 89 (4): 335–352.
... al. 2018b ). Yang et al. (2010) interpreted the Tarlong–Taodonggou area (southern Bogda Mountains) as half-graben, based on rapid lateral facies and thickness changes in the area, as well as basin geometries in seismic sections in the adjacent Turpan–Hami Basin. Our new studies in the northern...
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