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Listwanite

Listwanite is a 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 Listwanite rather than just read about it. In short: Listwanite (also sometimes spelled listvenite, listvanite, or listwaenite) is a rock type that forms when the groundmass of ultramafic rocks, most commonly mantle peridotites, is partially altered to carbonate minerals and cut by ubiquitous carbonate veins containing one or more of magnesite, calcite, dolomite, ankerite, and/or siderite. Original pyroxene and olivine in the peridotite are commonly altered to Mg- or…

Listwanite — main illustration
Listwanite — illustration

Key takeaways

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

Reference excerpt

Listwanite (also sometimes spelled listvenite, listvanite, or listwaenite) is a rock type that forms when the groundmass of ultramafic rocks, most commonly mantle peridotites, is partially altered to carbonate minerals and cut by ubiquitous carbonate veins containing one or more of magnesite, calcite, dolomite, ankerite, and/or siderite. Original pyroxene and olivine in the peridotite are commonly altered to Mg- or Ca-carbonate and hydrous Mg-silicates, such as serpentine and talc. Complete carbonation of peridotite means that every single atom of magnesium and calcium as well as some of the iron atoms have combined with CO2 to form secondary carbonate minerals such a magnesite, calcite, and siderite, while the remaining silica atoms, formerly found in pyroxene and olivine (prior to alteration), are found in quartz, serpentine, and talc. Thus, in terms of bulk mineralogy, listwanites consist primarily of quartz (often of a rusty red colour), carbonate, serpentine, talc, ± mariposite/fuchsite (i.e., Cr-bearing muscovite) ± gold.

Formation Geologists are still studying how listwanites form, but they likely form through the reaction of CO2-rich fluids with peridotites at approximately 50 to 200 °C. Faults and fractures permit the percolation of the CO2-rich fluids through peridotite, so the formation of listwanites is generally considered to be structurally controlled.

CO2 content Listwanites are important rocks to study for a number of reasons. First of all, listwanites contain large amounts of CO2 which originated from fluids that is now stored in solid mineral form. Recently, geologists and other scientists have been investigating the potential of storing CO2 in solid minerals (which are more stable than CO2 stored as a liquid or gas) through carbonation of mafic and ultramafic rocks. Mafic and ultramafic rocks take up significant CO2 through their natural alteration processes. However, the natural carbonation rates of these rocks are too slow to significantly offset anthropogenic CO2 emissions. Therefore, scientists are currently investigating if it is possible to geoengineer CO2 uptake in mafic and ultramafic rocks so that this CO2 uptake happens more quickly. This could be done, perhaps, by fracturing and heating and injection of CO2-rich fluids. This is already being tested in mafic basalts through the CarbFix Project in Iceland and ultramafic peridotite through 44.01 Project in the Semail Ophiolite of Oman. In addition to the recent interest in listwanites for carbon sequestration efforts, listwanites are also important because they are often associated with economic mineral deposits, particularly gold deposits.

See also Metasomatism

References

Illustrations

Listwanite: A quarry of listwanite in the region of Aosta Valley, in Italy
A quarry of listwanite in the region of Aosta Valley, in Italy
Listwanite: A quarry of listwanite in the region of Aosta Valley, in Italy
A quarry of listwanite in the region of Aosta Valley, in Italy

Worked examples

Example 1 — a first encounter with Listwanite

Start with the simplest possible case. Write down what Listwanite claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In 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 Listwanite 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 Listwanite 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 Listwanite

In research
Listwanite appears in 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 Listwanite 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
Listwanite is common in secondary-school and first-year university syllabi. It links to neighbouring topics Metamorphic rocks, Plutonic rocks, so understanding it makes those chapters shorter.
In everyday life
Look for Listwanite 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 Listwanite in 20 minutes

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

Frequently asked questions

What is Listwanite in simple terms?

Listwanite (also sometimes spelled listvenite, listvanite, or listwaenite) is a rock type that forms when the groundmass of ultramafic rocks, most commonly mantle peridotites, is partially altered to carbonate minerals and cut by ubiquitous carbonate veins containing one or more of magnesite, calci…

Why does Listwanite matter?

Because it connects several 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 Listwanite?

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 Listwanite.

Tags

  • Metamorphic rocks
  • Plutonic rocks

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