Jurassic climatic, lithofacies paleogeography map of Pan third pole

Guided by the theories of plate tectonics, paleogeography, petroliferous basin analysis and sedimentary basin dynamics, we have collected a large number of data and achievements of geological research and oil-gas geological research in Pan third pole in recent years, including basic materials such as stratum, sedimentation, paleontology, paleogeography, paleoenvironment, paleoclimate, structure, oil-gas (potash) geology, especially paleomagnetism and paleogenesis On the basis of zircon and geochemical data, combined with the results of typical measured stratigraphic sections, the lithofacies and climate palaeogeographic pattern of Jurassic period are restored and reconstructed, and the paleogeographic map of lithofacies and climate of Pan third extremely early, middle and late Jurassic (3 sheets) and pan third extremely early, middle and late Jurassic (3 sheets) are obtained, aiming to discuss paleogeography and paleostructure The control and influence of paleoclimate on oil and gas (including potash) resources, in order to reveal the geological conditions and resource distribution rules of oil and gas formation, and provide scientific basis and technical support for overseas and domestic oil and gas exploration and deployment in China.

Data file naming and use method

The map data is classified in the form of folders, for example, the folder name is "Pan third extremely early Jurassic climate paleogeographic map". The file contains "Pan third extremely early Jurassic climate paleogeographic map. JPG" and "Pan third extremely early Jurassic climate paleogeographic map. MXD" files. The rest are necessary engineering files. Double click "Pan third extremely early Jurassic climate paleogeographic map. MXD" to open a Rcmap, edit the map.

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Cite as:

LI Yalin. Jurassic climatic, lithofacies paleogeography map of Pan third pole. National Tibetan Plateau Data Center, 2020. doi: 10.11888/Paleoenv.tpdc.270419. (Download the reference: RIS | Bibtex )

Related Literatures:

1. Boucot, A. J., Xu, C., Scotese, C. R., & Morley, R. J. (2013). Phanerozoic paleoclimate: an atlas of lithologic indicators of climate.( View Details | Bibtex)

2. Cope, J. C. W., Ingham, J. K., & Rawson, P. F. (Eds.). (1999). Atlas of palaeogeography and lithofacies. Geological Society of London.( View Details | Bibtex)

3. Markello, J. R., Koepnick, R. B., Waite, L. E., Collins, J. F., Lukasik, J., & Simo, J. A. (2008). The carbonate analogs through time (CATT) hypothesis and the global atlas of carbonate fields—A systematic and predictive look at Phanerozoic carbonate systems. Controls on carbonate platform and reef development: SEPM Special Publication, 89, 15-45.( View Details | Bibtex)

4. Dercourt, J., Gaetani, M., Vrielynck, B., Barrier, E., Biju-Duval, B., Brunet, M. F., ... & Sandulescu, M. (2000). Peri-Tethys Palaeogeographical Atlas 2000. Université Pierre et Marie Curie, Paris.( View Details | Bibtex)

5. Scotese, C. R., & Golonka, J. (1997). Paleogeographic atlas (pp. 1-45). Arlington: PALEOMAP Project, University of Texas at Arlington.( View Details | Bibtex)

Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.

References literature

1.Golonka, J. (2007). Late Triassic and Early Jurassic palaeogeography of the world. Palaeogeography, Palaeoclimatology, Palaeoecology, 244(1-4), 297-307. (View Details )

2.Han, Z., Sinclair, H. D., Li, Y., Wang, C., Tao, Z., Qian, X., ... & Zhang, B. (2019). Internal drainage has sustained low‐relief Tibetan landscapes since the early Miocene. Geophysical Research Letters, 46(15), 8741-8752. (View Details )

3.Ning, Z., Zhang, L., Huntington, K. W., Wang, C., Dai, J., Han, Z., ... & Zhang, J. (2019). The burial and exhumation history of the Liuqu Conglomerate in the Yarlung Zangbo suture zone, southern Tibet: Insights from clumped isotope thermometry. Journal of Asian Earth Sciences, 174, 205-217. (View Details )

4.Golonka, J. (2004). Plate tectonic evolution of the southern margin of Eurasia in the Mesozoic and Cenozoic. Tectonophysics, 381(1-4), 235-273. (View Details )

5.Martin, A. Z. (2001). Late Permian to Holocene paleofacies evolution of the Arabian Plate and its hydrocarbon occurrences. GeoArabia, 6(3), 445-504. (View Details )

6.An, W., Hu, X., Garzanti, E., BouDagher-Fadel, M. K., Wang, J., & Sun, G. (2014). Xigaze forearc basin revisited (South Tibet): Provenance changes and origin of the Xigaze Ophiolite. Bulletin, 126(11-12), 1595-1613. (View Details )

7.Lai, W., Hu, X., Garzanti, E., Sun, G., Garzione, C. N., BouDagher Fadel, M., & Ma, A. (2019). Initial growth of the Northern Lhasaplano, Tibetan Plateau in the early Late Cretaceous (ca. 92 Ma). Bulletin, 131(11-12), 1823-1836. (View Details )

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Geographic coverage
East: 180.00 West: 180.00
South: 90.00 North: 90.00
  • Temporal resolution: 1000 year < x
  • Spatial resolution: 100km - 1000km
  • File size: 96 MB
  • Browse count: 2,705 Times
  • Apply count: 8 Times
  • Share mode: online
  • Temporal coverage: 195-150 million years
  • Updated time: 2020-03-10
Contact Information
: LI Yalin  

Distributor: National Tibetan Plateau Data Center

Email: data@itpcas.ac.cn

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