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Summarized Content

textbook on applied numerical methods: plate tectonics, subduction, mantle convection and planetary models. textbook provides user-friendly introduction to applied numerical methods  for graduate students and researchers working in the fields. modelling of geological processes numerically was for a long time considered as a complex research domain of high-level mathematicians and geophysicists with strong experience in numerical methods. now, for the first time, students and researchers in geology and natural sciences can learn this subject from a single, accessible textbook. it only requires minimal mathematical background (derivatives and simple the first part of this textbook gradually introduces relevant partial differential equations of continuum mechanics and explains in details numerical methods applied for their solution. the second part contains reader-friendly introduction into state-of-the-art visco-elasto-plastic thermo-mechanical geodynamic modelling. this textbook does not only present numerical methods but also provides insight into the modelling of  major geological processes. numerical examples include models of subduction, lithospheric extension, continental collision, slab break-off, intrusion emplacement, mantle convection and planetary core formation. 47 exercises and 67 matlab programs allow readers to test their. understanding and experiment with numerical methods and models.. mars is certainly more accessible planet than venus and its surface is studied in much more details. however, surface of venus seems to be. much more exciting geologically and expose many large-scale features of enigmatic origin, such as coronae and novae. venus coronae are 513 approximately circular structures that range in diameter from 60 km to 2000  km. coronae typically have a raised rim centers’’ 100–300 km in diameter, 64 have been identified. in contrast to volcanoes, novae show a dominance of tectonic activity (e.g., surface fracturing) over volcanic activity. origin of both novae and coronae is often explained by an interaction of the venus


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Title: Introduction to numerical methods for geologists, mathematicians and physicists | Textbook on applied numerical methods: plate tectonics, subduction, mantle convection and planetary
Description: Textbook on applied numerical methods: plate tectonics, subduction, mantle convection and planetary
H1: Introduction to numerical methods for geologists, mathematicians and physicists
H2: Textbook on applied numerical methods: plate tectonics, subduction, mantle convection and planetary models
H3: Introduction to Applied Numerical Methods February 3, 2010

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/about/:
Title

Why did I write this textbook? | Introduction to numerical methods for geologists, mathematicians and physicists

Description

There were two main reasons. First - I suffered a lot when I started to learn this subject since no simple introductory textbook written specifically for Earth scientists was available. I was collecting pieces of information here  and there - in various books, papers and (most important way) from many conversations with other modelers. This…

H1

Introduction to numerical methods for geologists, mathematicians and physicists

H2

Textbook on applied numerical methods: plate tectonics, subduction, mantle convection and planetary models

H3

Why did I write this textbook? February 3, 2010

/2010/02/03/hello-world/:
Title

Introduction to Applied Numerical Methods | Introduction to numerical methods for geologists, mathematicians and physicists

Description

This textbook provides user-friendly introduction to applied numerical methods  for graduate students and researchers working in the fields of geology, mathematics and physics. Modelling of geological processes numerically was for a long time considered as a complex research domain of high-level mathematicians and geophysicists with strong experience in numerical methods. Now, for the first time,…

H1

Introduction to numerical methods for geologists, mathematicians and physicists

H2

Textbook on applied numerical methods: plate tectonics, subduction, mantle convection and planetary models

H3

Introduction to Applied Numerical Methods February 3, 2010

/category/numerical-methods/:
Title

numerical methods | Introduction to numerical methods for geologists, mathematicians and physicists

Description

Posts about numerical methods written by tgerya

H1

Introduction to numerical methods for geologists, mathematicians and physicists

H2

Textbook on applied numerical methods: plate tectonics, subduction, mantle convection and planetary models

H3

Porous water enables subduction initiation November 4, 2013

/2014/03/15/venus-vs-mars-what-planet-is-more-geologically-exciting/:
Title

Venus vs. Mars: what planet is more geologically exciting? | Introduction to numerical methods for geologists, mathematicians and physicists

Description

Mars is certainly more accessible planet than Venus and its surface is studied in much more details. However, surface of Venus seems to be much more exciting geologically and expose many large-scale features of enigmatic origin, such as coronae and novae Venus coronae are 513 approximately circular structures that range in diameter from 60 km…

H1

Introduction to numerical methods for geologists, mathematicians and physicists

H2

Textbook on applied numerical methods: plate tectonics, subduction, mantle convection and planetary models

H3

Venus vs. Mars: what planet is more geologically exciting? March 15, 2014

/category/uncategorized/:
Title

Uncategorized | Introduction to numerical methods for geologists, mathematicians and physicists

Description

Posts about Uncategorized written by tgerya

H1

Introduction to numerical methods for geologists, mathematicians and physicists

H2

Textbook on applied numerical methods: plate tectonics, subduction, mantle convection and planetary models

H3

Venus vs. Mars: what planet is more geologically exciting? March 15, 2014

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