Collision Tectonics (9 results)
Published by 1986, 1986
- Softcover
Seller: Wissenschaftliches Antiquariat Köln Dr. Sebastian Peters UG, Köln, GermanyWissenschaftliches Antiquariat Köln Dr. Sebastian Peters UG
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Add to basketgeheftet, ohne Einband. Condition: gut. 24 cm, Besitzvermerk, aus der Sammlung Alexander Tollmann. Sprache: eng.
Published by Academic Journal Offprint from: - Journal of the Geological Society, Volume 161, Part 5, September 2004., 2004
Seller: Nar Valley Books & Prints, King's Lynn, United KingdomNar Valley Books & Prints
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Add to basket14pp, 9 figs, Printed Card Cover, VGC.

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Seller: Richard Sylvanus Williams (Est 1976), WINTERTON, United KingdomRichard Sylvanus Williams (Est 1976)
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Hardback. Condition: VG. No DW. 1st Edition. Book is in very good condition with minor signs of wear and/or age. SPECIAL POSTAGE RATES MAY APPLY Packed weight 1200g.

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Seller: Acanthophyllum Books, Holywell, FLINT, United KingdomAcanthophyllum Books
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Hard covers, dust jacket. Condition: Fine. Dust Jacket Condition: Fine. 1st edition. Scarcely used. Owner's ink stamp. Weight: 1.0 Language: English.
Published by London, The Geological Society, 2011, 2011
- Hardcover
- First Edition
Seller: Grant's Bookshop, Cheltenham, VIC, AustraliaGrant's Bookshop
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Add to basketOctavo, vi+382 pages, original boards, a very good copy. First edition.

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Hardcover. Condition: New. NEW. SHIPS FROM MULTIPLE LOCATIONS. book.

- Softcover
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Seller: AHA-BUCH GmbH, Einbeck, GermanyAHA-BUCH GmbH
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Taschenbuch. Condition: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - Please note that the content of this book primarily consists of articlesavailable from Wikipedia or other free sources online. The Molucca SeaCollision Zone is postulated by paleogeologists to explain the tectonicsof the area based on the Molucca Sea in Indonesia, and adjacent involvedareas. The Molucca Sea Collision Zone is the site of an orthogonalcollision between two active subduction systems. Both the Halmaherasubduction system to the east, and the Sangihe subduction system to thewest, have subducted oceanic lithosphere of the Molucca Sea plate, whichhas been completely consumed, with the Sangihe arc now over-riding theHalmahera forearc. Both volcanic arcs have been active since theNeogene. Both arcs show increased evidence for sediment recycling as thecollision progressed, but for differing reasons.…

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Seller: preigu, Osnabrück, Germanypreigu
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Taschenbuch. Condition: Neu. Maluku Islands | Archipelago, Malay Archipelago, Tectonics, Halmahera Plate, Molucca Sea Collision Zone, Sulawesi, Celebes, Timor, Sago, Rice, Nutmeg, Clove, Melanesia, Banda Islands, Austronesian languages | Frederic P. Miller (u. a.) | Taschenbuch | Englisch | 2026 | OmniScriptum | EAN 9786130270551 | Verantwortliche Person für die EU: preigu GmbH & Co. KG, Lengericher Landstr. 19, 49078 Osnabrück, mail[at]preigu[dot]de | Anbieter: preigu Print on Demand.…

Published by Omniscriptum
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Seller: AHA-BUCH GmbH, Einbeck, GermanyAHA-BUCH GmbH
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Taschenbuch. Condition: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - Please note that the content of this book primarily consists of articlesavailable from Wikipedia or other free sources online. Continentalcollision is a phenomenon of the plate tectonics of Earth that occurs atconvergent boundaries. Continental collision is a variation on thefundamental process of subduction, whereby the subduction zone isdestroyed, mountains produced, and two continents sutured together.Continental collision is known only from this planet and is aninteresting example of how our different crusts, oceanic andcontinental, behave during subduction. Continental collision is not aninstantaneous event, like a car crash, but may take several tens ofmillions of years before the faulting and folding caused by collisionstop. Collision between India and Asia has been going on for about 50million years already and shows no signs of abating. Collision betweenEast and West Gondwana to form the East African Orogen took about 100million years from beginning (610 Ma) to end (510 Ma). Collision betweenGondwana and Laurasia to form Pangea occurred in a relatively briefinterval, about 50 million years long.…