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Glaciogenic Reservoir Analogue Studies Project

Glaciogenic Reservoir Analogue Studies Project is a physics 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 Glaciogenic Reservoir Analogue Studies Project rather than just read about it. In short: The Glaciogenic Reservoir Analogue Studies Project (GRASP) is a research group studying the subglacial to proglacial record of Pleistocene glacial events. It is based in the Delft University of Technology.

Key takeaways

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

Reference excerpt

The Glaciogenic Reservoir Analogue Studies Project (GRASP) is a research group studying the subglacial to proglacial record of Pleistocene glacial events. It is based in the Delft University of Technology.

Introduction to glaciogenic reservoirs Glaciogenic reservoirs are sedimentary rocks deposited under an ice sheet influence and that are involved into a gas or oil reservoir. The glacial earth system is complex to study. A large amount on past and ongoing scientific programs work(ed) on our cryosphere and generate a lot of debate about its dynamic, sustainability and behavior against climate changes. Past glaciations or ice ages record occurred several times (Timeline of glaciation) along the geological time scale. As they are hundreds of million years old, these ancient glaciations are even more hard to analyse and study. Earth at that time had a different atmosphere composition, the chemistry of the oceans was also different, life evolution on earth had also a great impact on the dynamic of these ice sheets, the continents were in a particular setting, etc. Geologists have a broad idea of all those parameters but glaciologists know that this is the combination of those setting that bring to our current ice-age. A glacial system is able to produce a very large amount of sediment due to the tremendous erosive forces of ice at its base. Those sediments are particularly coarse-grained (principally sandstones and conglomerates) and produced in consequent volumes [1]. For their good reservoir properties, ancient glacially-related sediments have been targeted by oil industries. They are currently massively exploited in North Africa, in the Arabic peninsula, South Africa, and few small fields are present in Asia, Australia and Northern Europe. The main ice ages concerned are the Late Ordovician glaciation (Hirnantian) and the Permo-Carboniferous glaciations.

Project objectives Analogy is a usual geologist method, using the present day observations and project/adapt it to the ancient earth systems. The main problem of this technique is the time-scale considered and the observation methods used. Most of the time, observations of active ice-sheet processes are instantaneous at geological time-scale and hard to apply in the ancient. Furthermore, in the ancient, field and geophysical studies are carried out at lower resolution but on a wider scale (time and space). Finally, even if Subglacial lakes are observed below ice sheets, melt-water drainage system processes ongoing, especially like the tunnel valleys remain unobserved directly. The record of these huge subglacial "rivers" is mainly analysed via the recent ice ages imprints (Weichselian, Saalian and Pre-Illinoian or Elsterian stages) and in the ancient one (Late Ordovician and Permo-Carboniferous). The idea of GRASP is to use methods commonly applied in the ancient onto recent glaciation record (Pleistocene). In the ancient, wide datasets are acquired by oil companies during exploration of sedimentary basins. By using the same type of data for the Pleistocene glacial record, the project tries to generate data comparable in between ancient and recent glaciations. The studied area is the North Sea that was glaciated during the Last Glacial Maximum as well as the Northwestern Europe. On the sea floor, around the North Sea and into the kilometre of sediments below, many traces and evidences of the glacial events are recorded. As this place is a petroleum province, many data, especially geophysics ones are currently released or could be borrowed for academic purposes. So, by joining the skills of three different universities, with the help of many data providers and the funding of six oil companies, new income is made into the knowledge of paleo-glacial systems. Basin analysis containing geophysical, reservoir and sedimentological models are produced in a new way and in a new type of environment. In an economic point of view, oil companies are interested in these models to have comparable data with their oil fields. In an academic one, understanding the recent ice sheet dynamic and its associated subglacial meltwater flow is crucial in the context of climate changes or fundamentally solving the intricate glacial record equation of recent and past ice ages.

See also Climate change (modern day) Climate change (general concept)

References

External links GRASP website Archived 2011-07-24 at the Wayback Machine Palaeos:Late Ordovician Age IUGS/UNESCO: IGCP 503 ECORD: sedimentary basins

Worked examples

Example 1 — a first encounter with Glaciogenic Reservoir Analogue Studies Project

Start with the simplest possible case. Write down what Glaciogenic Reservoir Analogue Studies Project claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In physics, 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 Glaciogenic Reservoir Analogue Studies Project 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 Glaciogenic Reservoir Analogue Studies Project 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 Glaciogenic Reservoir Analogue Studies Project

In research
Glaciogenic Reservoir Analogue Studies Project appears in physics 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 Glaciogenic Reservoir Analogue Studies Project 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
Glaciogenic Reservoir Analogue Studies Project is common in secondary-school and first-year university syllabi. It links to neighbouring topics Delft University of Technology, Geophysics organizations, Glaciology, so understanding it makes those chapters shorter.
In everyday life
Look for Glaciogenic Reservoir Analogue Studies Project 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 Glaciogenic Reservoir Analogue Studies Project in 20 minutes

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

Frequently asked questions

What is Glaciogenic Reservoir Analogue Studies Project in simple terms?

The Glaciogenic Reservoir Analogue Studies Project (GRASP) is a research group studying the subglacial to proglacial record of Pleistocene glacial events. It is based in the Delft University of Technology.

Why does Glaciogenic Reservoir Analogue Studies Project matter?

Because it connects several physics 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 Glaciogenic Reservoir Analogue Studies Project?

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 Glaciogenic Reservoir Analogue Studies Project.

Tags

  • Delft University of Technology
  • Geophysics organizations
  • Glaciology
  • Oil reserves
  • Sedimentology

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