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Skagerrak-Centered Large Igneous Province

Skagerrak-Centered Large Igneous Province 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 Skagerrak-Centered Large Igneous Province rather than just read about it. In short: The Skagerrak-Centered Large Igneous Province (SCLIP), also known as the European-Northwest African Large Igneous Province (EUNWA), and Jutland LIP, is a 300 million year old (Ma) large igneous province (LIP) centered on what is today the Skagerrak strait in north-western Europe (57°50′N 9°04′E, paleocoordinates 11°N 16°E (south of Lake Chad)). It was named by Torsvik et al. 2008.

Key takeaways

  • Skagerrak-Centered Large Igneous Province 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 Skagerrak-Centered Large Igneous Province to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Skagerrak-Centered Large Igneous Province from memory before moving on to harder problems.

Reference excerpt

The Skagerrak-Centered Large Igneous Province (SCLIP), also known as the European-Northwest African Large Igneous Province (EUNWA), and Jutland LIP, is a 300 million year old (Ma) large igneous province (LIP) centered on what is today the Skagerrak strait in north-western Europe (57°50′N 9°04′E, paleocoordinates 11°N 16°E (south of Lake Chad)). It was named by Torsvik et al. 2008. The SCLIP covered an area of at least 0.5×10^6 km2 (0.19×10^6 sq mi) and includes the Oslo and Skagerrak grabens, areas in south-western Sweden, Scotland, northern England, and the central North Sea. The SCLIP erupted at 297±4 Ma. It produced 228,000 km2 of currently exposed volcanic material that can be found in Skagerrak, the Oslo Fjord, central North Sea, North-east Germany; 14,000 km2 of sills in Scotland, England, Germany, The Netherlands, and Sweden; and 3,353 km total length of dykes in Scotland, Norway, and Sweden. The period of eruptions comprised a relatively short time span, perhaps less than 4 Ma, but magma propagated more than 1,000 km (620 mi) from the plume centre. Plumes derived from a superplume (or Large Low Shear Velocity Province (LLSVP)) overlay the boundary of the superplume at the core-mantle boundary (CMB). To test whether the SCLIP met these criteria, Torsvik et al. used a shear-wave tomographic model of the mantle, in which the SCLIP indeed do project down to the margin of the African superplume at the CMB at a depth of 2800 km. A series of LIPs are associated with the African superplume, of which the SCLIP is the oldest: SCLIP (300 Ma), Bachu (275 Ma), Emeishan (260 Ma), Siberian (250 Ma), and Central Atlantic (200 Ma). It is possible that these plumes together caused the break-up of Pangaea and therefore play an important role in the supercontinent cycle. The SCLIP is associated with the Moscovian and Kasimovian stages of the Carboniferous rainforest collapse around 296-310 Ma together with the Siberian Barguzin-Vitim LIP.

See also Avalonia List of flood basalt provinces Central Atlantic magmatic province, Late Triassic to Early Jurassic igneous province in the area Central Skåne Volcanic Province, Early Jurassic to Early Cretaceous igneous province in southern Sweden

References

Bibliography

Worked examples

Example 1 — a first encounter with Skagerrak-Centered Large Igneous Province

Start with the simplest possible case. Write down what Skagerrak-Centered Large Igneous Province 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 Skagerrak-Centered Large Igneous Province 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 Skagerrak-Centered Large Igneous Province 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 Skagerrak-Centered Large Igneous Province

In research
Skagerrak-Centered Large Igneous Province 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 Skagerrak-Centered Large Igneous Province 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
Skagerrak-Centered Large Igneous Province is common in secondary-school and first-year university syllabi. It links to neighbouring topics Asselian, Carboniferous volcanism, Geology of Denmark, so understanding it makes those chapters shorter.
In everyday life
Look for Skagerrak-Centered Large Igneous Province 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 Skagerrak-Centered Large Igneous Province in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Skagerrak-Centered Large Igneous Province 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 Skagerrak-Centered Large Igneous Province out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Skagerrak-Centered Large Igneous Province in simple terms?

The Skagerrak-Centered Large Igneous Province (SCLIP), also known as the European-Northwest African Large Igneous Province (EUNWA), and Jutland LIP, is a 300 million year old (Ma) large igneous province (LIP) centered on what is today the Skagerrak strait in north-western Europe (57°50′N 9°04′E, pa…

Why does Skagerrak-Centered Large Igneous Province 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 Skagerrak-Centered Large Igneous Province?

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 Skagerrak-Centered Large Igneous Province.

Tags

  • Asselian
  • Carboniferous volcanism
  • Geology of Denmark
  • Geology of England
  • Geology of Norway
  • Geology of Scotland
  • Geology of Sweden
  • Geology of the Netherlands
  • Geology of the North Sea
  • Gzhelian
  • Large igneous provinces
  • Paleozoic Denmark

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