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Tektonik

Tektonik (dari bahasa Yunani Kuno τεκτονικός tektonikós yang artinya "berkaitan dengan konstruksi", melalui bahasa Latin tectonicus)^[1] adalah proses yang menghasilkan struktur dan sifat kerak bumi dan evolusinya dari waktu ke waktu. Bidang tektonik planet memperluas konsep ini ke planet dan bulan lain.^[2]^[3]

Proses-proses ini meliputi pembentukan gunung; pertumbuhan dan perilaku inti benua yang kuat dan tua yang dikenal sebagai "kraton"; dan cara lempeng-lempeng yang relatif kaku, yang membentuk lapisan luar bumi berinteraksi satu sama lain. Prinsip-prinsip tektonik juga memberikan kerangka kerja untuk memahami sabuk gempa bumi dan sabuk vulkanik yang secara langsung memengaruhi sebagian besar populasi global.

Studi tektonik penting sebagai panduan bagi ahli geologi ekonomi yang mencari bahan bakar fosil dan endapan bijih sumber daya logam dan nonlogam. Pemahaman tentang prinsip-prinsip tektonik dapat membantu ahli geomorfologi untuk menjelaskan pola erosi dan fitur permukaan Bumi lainnya.^[4]

Jenis-jenis utama rezim tektonik

Tektonika lempeng

Bidang studi tektonik lainnya

Referensi

^ Harper, Douglas. "tectonic". Online Etymology Dictionary.
^ Geologists (as distinct from architects) may define tectonics as "the architecture of the Earth's crust" - O'Hara, Kieran D. (19 April 2018). A Brief History of Geology. Cambridge: Cambridge University Press. ISBN 9781107176188. Diakses tanggal 23 March 2023. The words tectonics and architecture are derived from the same Greek root, and tectonics is defined as the architecture of the Earth's crust.
^ Watters, Thomas R.; Schultz, Richard A. (2010). "Planetary tectonics: introduction". Dalam Watters, Thomas R.; Schultz, Richard A. (ed.). Planetary Tectonics. Cambridge Planetary Science, ISSN 0265-3044 – Volume 11. Cambridge: Cambridge University Press. hlm. 2. ISBN 9780521765732. Diakses tanggal 23 March 2023. Since the 1960s, an armada of exploratory spacecraft have identified widespread evidence of tectonism on all the terrestrial planets, most of the satellites of the outer planets, and on a number of asteroids. Tectonic landforms on large and small bodies in the solar system are as ubiquitous as impact craters.
^ Anderson, Robert S.; Burbank, Douglas W. (2 November 2011) [2001]. "Rates of erosion and uplift". Tectonic Geomorphology (Edisi 2). Chichester, West Sussex: John Wiley & Sons. ISBN 9781444345049. Diakses tanggal 23 March 2023.

Bacaan lanjutan

Edward A. Keller (2001) Active Tectonics: Earthquakes, Uplift, and Landscape Prentice Hall; 2nd edition, ISBN 0-13-088230-5
Stanley A. Schumm, Jean F. Dumont and John M. Holbrook (2002) Active Tectonics and Alluvial Rivers, Cambridge University Press; Reprint edition, ISBN 0-521-89058-6
B.A. van der Pluijm and S. Marshak (2004). Earth Structure – An Introduction to Structural Geology and Tectonics. 2nd edition. New York: W.W. Norton. hlm. 656. ISBN 0-393-92467-X. Diarsipkan dari asli tanggal 3 May 2017. Diakses tanggal 31 October 2008.

Pranala luar

[1] Harper, Douglas. "tectonic". Online Etymology Dictionary.

[2] Geologists (as distinct from architects) may define tectonics as "the architecture of the Earth's crust" - O'Hara, Kieran D. (19 April 2018). A Brief History of Geology. Cambridge: Cambridge University Press. ISBN 9781107176188. Diakses tanggal 23 March 2023. The words tectonics and architecture are derived from the same Greek root, and tectonics is defined as the architecture of the Earth's crust.

[Watters_etal_2010-3] Watters, Thomas R.; Schultz, Richard A. (2010). "Planetary tectonics: introduction". Dalam Watters, Thomas R.; Schultz, Richard A. (ed.). Planetary Tectonics. Cambridge Planetary Science, ISSN 0265-3044 – Volume 11. Cambridge: Cambridge University Press. hlm. 2. ISBN 9780521765732. Diakses tanggal 23 March 2023. Since the 1960s, an armada of exploratory spacecraft have identified widespread evidence of tectonism on all the terrestrial planets, most of the satellites of the outer planets, and on a number of asteroids. Tectonic landforms on large and small bodies in the solar system are as ubiquitous as impact craters.

[4] Anderson, Robert S.; Burbank, Douglas W. (2 November 2011) [2001]. "Rates of erosion and uplift". Tectonic Geomorphology (Edisi 2). Chichester, West Sussex: John Wiley & Sons. ISBN 9781444345049. Diakses tanggal 23 March 2023.

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