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Subashi Formation

Subashi Formation is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Subashi Formation rather than just read about it. In short: The Subashi Formation (Chinese: 苏巴什组) is a Late Cretaceous (Campanian to Maastrichtian) formation from the Xinjiang Autonomous Region of western China. Initially described by Dong Zhiming in 1977, the formation contains remains of Tarbosaurus which were initially described as a separate taxon Shanshanosaurus huoyanshanensis.

Key takeaways

  • Subashi Formation belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Subashi Formation to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Subashi Formation from memory before moving on to harder problems.

Reference excerpt

The Subashi Formation (Chinese: 苏巴什组) is a Late Cretaceous (Campanian to Maastrichtian) formation from the Xinjiang Autonomous Region of western China. Initially described by Dong Zhiming in 1977, the formation contains remains of Tarbosaurus which were initially described as a separate taxon Shanshanosaurus huoyanshanensis. Remains of a sauropod, likely Nemegtosaurus, and a hadrosaurid, likely Jaxartosaurus, have also been found. The formation is located in the Flaming Mountains region of Xinjiang, north of the Turpan Depression. It is not far from Lianmuqin Town of Shanshan County, and is presumably named after the village of Subashi (42°55′11″N 89°44′36″E), which is located some 15 kilometres (9.3 mi) to the west of Lianmuqin, in Tuyugou Township (吐峪沟乡).

Fossil content The following fossils were reported from the formation:

Dinosaurs

Ornithischians

Sauropods

Theropods

Turtles

Oofossils

See also Subashi (lost city)

References

Bibliography Xi, D.; Wan, X.; Li, G.; Li, G. (2018), "Cretaceous integrative stratigraphy and timescale of China", Science China Earth Sciences, 61: 1–31, doi:10.1007/s11430-017-9262-y Zhang, S.-K.; Wang, Q. (2010), "A new species of ovaloolithids from Turpan Basin in Xinjiang, China", Vertebrata PalAsiatica, 48: 71–75 Glut, Donald F (2001), Dinosaurs, the encyclopedia: Supplement, Volume 1, McFarland & Co., p. 497, ISBN 078641166X Dong, Z (1997), On a large claw of sauropod from the Upper Cretaceous in the Turpan Basin, Xinjiang, China. In Z. Dong (ed.), Sino-Japanese Silk Road Dinosaur Expedition China Ocean Press, Beijing, pp. 111–112 Dauphin, Y (1994), "Comparaison des microstructures et de la composition chimique de coquilles d'oeufs fossiles du Sud de la France, de quelques specimens d'Asie et d'oiseaux actuels", Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen, 194: 55–71, doi:10.1127/njgpa/194/1994/55 Shen, Y.-b.; Mateer, N. J. (1992), An outline of the Cretaceous System in northern Xinjiang, western China. In N. J. Mateer, P.-j. Chen (eds.), Aspects of Nonmarine Cretaceous Geology China Ocean Press, Beijing, pp. 50–77 Zhai, R.-j.; Zheng, J.-j.; Tong, Y.-s. (1978), "Stratigraphy of the mammal-bearing Tertiary of the Turfan Basin, Sinkiang", Reports of Paleontological Expedition to Sinkiang. III. Permian and Triassic Vertebrate Fossils of Dzungaria Basin and Tertiary Stratigraphy and Mammalian Fossils of Turfan Basin, 13: 68–81 Dong, Z (1977), "On the dinosaurian remains from Turpan, Xinjiang", Vertebrata PalAsiatica, 15: 59–66 Yeh, H (1974), "A new fossil dermatemydid from Sinkiang", Vertebrata PalAsiatica, 12: 257–261 Young, C.-C (1965), "Fossil eggs from Nanshiung, Kwangtung and Kanchou, Kiangsi", Vertebrata PalAsiatica, 9: 141–170

Worked examples

Example 1 — a first encounter with Subashi Formation

Start with the simplest possible case. Write down what Subashi Formation claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Subashi Formation before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Subashi Formation ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Subashi Formation

In research
Subashi Formation appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Subashi Formation in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Subashi Formation is common in secondary-school and first-year university syllabi. It links to neighbouring topics Campanian Stage, Geologic formations of China, Maastrichtian Stage, so understanding it makes those chapters shorter.
In everyday life
Look for Subashi Formation outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.

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How to study Subashi Formation in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Subashi Formation means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Subashi Formation out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Subashi Formation in simple terms?

The Subashi Formation (Chinese: 苏巴什组) is a Late Cretaceous (Campanian to Maastrichtian) formation from the Xinjiang Autonomous Region of western China. Initially described by Dong Zhiming in 1977, the formation contains remains of Tarbosaurus which were initially described as a separate taxon Shans…

Why does Subashi Formation matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Subashi Formation?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Subashi Formation.

Tags

  • Campanian Stage
  • Geologic formations of China
  • Maastrichtian Stage
  • Mudstone formations of China
  • Ooliferous formations
  • Paleontology in Xinjiang
  • Sandstone formations
  • Upper Cretaceous Series of Asia

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