> endobj 13 0 obj << /ProcSet [ /PDF /Text ] /ColorSpace << /Cs1 23 0 R >> /Font << /F1.0 21 0 R /F2.0 14 0 R /F5.0 31 0 R /F3.0 16 0 R /F7.0 34 0 R /F4.0 27 0 R /F6.0 33 0 R >> >> endobj 14 0 obj << /Type /Font /Subtype /TrueType /BaseFont /RFNJXW+Palatino-Roman /FontDescriptor 20 0 R /Widths 17 0 R /FirstChar 0 /LastChar 255 /Encoding /MacRomanEncoding >> endobj 15 0 obj << /Type /FontDescriptor /Ascent 914 /CapHeight 0 /Descent -236 /Flags 32 /FontBBox [ -150 -236 823 915 ] /FontName /NJCQOV+TremorITC /ItalicAngle 0 /StemV 0 /MaxWidth 1000 /FontFile2 58 0 R >> endobj 16 0 obj << /Type /Font /Subtype /TrueType /BaseFont /NJCQOV+TremorITC /FontDescriptor 15 0 R /Widths 22 0 R /FirstChar 0 /LastChar 255 /Encoding /MacRomanEncoding >> endobj 17 0 obj [ 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 250 278 372 606 500 840 778 209 334 334 390 606 250 334 250 606 500 500 500 500 500 500 500 500 500 500 250 250 606 606 606 444 748 778 611 709 774 611 557 764 833 337 334 727 611 946 832 787 605 787 668 525 613 778 723 1000 667 667 667 334 606 334 606 500 334 500 554 444 611 480 334 557 583 292 234 557 292 883 583 546 602 561 396 424 327 604 565 834 517 557 500 334 606 334 606 750 778 778 709 611 832 787 778 500 500 500 500 500 500 444 480 480 480 480 288 288 288 288 583 546 546 546 546 546 604 604 604 604 500 400 500 500 500 606 628 557 748 748 980 334 334 750 944 834 750 549 750 750 500 577 750 750 750 750 750 334 334 750 758 557 444 278 606 750 500 750 750 500 500 1000 250 778 778 787 999 828 500 1000 500 500 278 278 549 750 557 667 167 745 332 332 605 608 500 250 278 500 1145 778 611 778 611 611 337 337 337 337 787 787 750 787 778 778 778 288 334 334 334 334 250 334 334 380 313 334 ] endobj 18 0 obj << /Type /FontDescriptor /Ascent 701 /CapHeight 0 /Descent -299 /Flags 32 /FontBBox [ -167 -299 1063 828 ] /FontName /HCHHXU+Symbol /ItalicAngle 0 /StemV 0 /MaxWidth 1042 /FontFile2 44 0 R >> endobj 19 0 obj [ 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 250 334 713 500 549 834 778 439 334 334 500 549 250 549 250 278 500 500 500 500 500 500 500 500 500 500 278 278 549 549 549 444 549 723 667 723 612 611 764 604 723 334 631 723 687 890 723 723 769 742 557 592 611 690 439 769 646 795 611 334 863 334 659 500 517 631 549 549 495 439 521 412 604 330 604 549 549 577 521 549 549 521 549 604 439 577 713 687 494 687 495 480 201 480 549 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 601 745 621 248 549 167 713 500 753 753 753 753 1042 987 601 987 604 601 549 601 601 549 713 601 601 601 601 601 549 1000 601 1000 659 824 687 795 601 769 601 601 769 769 713 250 713 713 713 713 713 769 713 791 791 891 824 549 601 713 604 604 1042 987 604 987 604 495 330 791 791 787 713 384 384 384 384 384 384 495 495 495 495 601 330 274 687 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406 406 406 406 406 381 363 363 363 363 250 250 250 250 412 385 385 385 385 385 397 397 397 397 331 314 387 462 418 258 477 440 379 833 409 500 500 500 745 527 500 833 500 500 443 527 500 500 500 500 500 394 271 500 580 363 403 260 833 500 577 500 500 349 333 495 152 496 496 520 684 559 478 592 271 259 138 125 833 500 389 472 141 606 190 202 541 563 385 172 125 261 857 496 423 496 423 423 264 264 264 264 520 520 500 520 481 481 481 250 500 500 500 500 500 500 500 500 500 500 ] endobj 23 0 obj [ /ICCBased 46 0 R ] endobj 24 0 obj << /Length 25 0 R /Filter /FlateDecode >> stream Washington, D.C. 1910 (see especially pages 16-28). 0000042537 00000 n 0000048214 00000 n Similarly, the crust of the earth can gradually elastic rebound theoryTheory which holds that accumulated potential energy, stored as elastic strains, is released by faulting (i.e. x��W�r�H}���G��!�Aysmy/Y����*/����!3`��~� "�L�e@�g�O�9���'81��eǶAB�y����_(�ív �`����m����{�c��Q�C�ç�N����g�6,r��c���b W�=�{�0_�� H��"�ø:H���T��/��u~ �m�������ǧ�A�'����\�6K�VR�p[+%�:��a. 0000048235 00000 n In these subduction zones, friction causes the top plate to bend and store elastic energy. 0000049054 00000 n Such irregular properties of fault rupture are now included in the modeling of earthquake sources, both physically and mathematically. 0000001477 00000 n 10 0 obj << /Linearized 1 /O 12 /H [ 1477 249 ] /L 139390 /E 130839 /N 2 /T 139072 >> endobj xref 10 53 0000000016 00000 n The following diagram illustrates the process. - Definition & Location, Accretionary Wedge: Definition & Formation, Biological and Biomedical For more information, see the following related content on ScienceDaily: Content on this website is for information only. 0000002253 00000 n 0000011412 00000 n Reid, H.F., The Mechanics of the Earthquake, The California Start at the bottom. Elastic rebound, as demonstrated by a rubber band, is an important concept to understand when studying earthquakes and their effects. 0000005421 00000 n These observations provided the basis for the landmark "theory of elastic rebound", introduced by Professor H.F. Reid of Johns Hopkins University, who served on Lawson's Commission. In geology, the elastic rebound theory was the first theory to satisfactorily explain earthquakes. In dip-slip faults, if the hanging-wall block moves downward relative to the footwall block, it is called “normal” faulting; the opposite motion, with the hanging wall moving upward relative to the footwall, produces reverse or thrust faulting. It is estimated that only 10 percent or less of an earthquake's total energy is radiated as seismic energy. The usual fault model has a “strike” (that is, the direction from north taken by a horizontal line in the fault plane) and a “dip” (the angle from the horizontal shown by the steepest slope in the fault). The actual faulting associated with an earthquake may be complex, and it is often not clear whether in a particular earthquake the total energy issues from a single fault plane. Once there is a lot of elastic energy stored, you can let it go. Youtube 映画 無料 洋画, Most Afl Premierships Player List, Blitzer Introductory And Intermediate Algebra, What To Do When You Miss Him, Terry Riley Liverpool, Steve Skrovan Net Worth, Catholic Genuflecting Rules, Poppy Harlow Wedding, " />

elastic rebound theory steps

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/MacRomanEncoding >> endobj 17 0 obj [ 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 750 250 278 372 606 500 840 778 209 334 334 390 606 250 334 250 606 500 500 500 500 500 500 500 500 500 500 250 250 606 606 606 444 748 778 611 709 774 611 557 764 833 337 334 727 611 946 832 787 605 787 668 525 613 778 723 1000 667 667 667 334 606 334 606 500 334 500 554 444 611 480 334 557 583 292 234 557 292 883 583 546 602 561 396 424 327 604 565 834 517 557 500 334 606 334 606 750 778 778 709 611 832 787 778 500 500 500 500 500 500 444 480 480 480 480 288 288 288 288 583 546 546 546 546 546 604 604 604 604 500 400 500 500 500 606 628 557 748 748 980 334 334 750 944 834 750 549 750 750 500 577 750 750 750 750 750 334 334 750 758 557 444 278 606 750 500 750 750 500 500 1000 250 778 778 787 999 828 500 1000 500 500 278 278 549 750 557 667 167 745 332 332 605 608 500 250 278 500 1145 778 611 778 611 611 337 337 337 337 787 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601 549 601 601 549 713 601 601 601 601 601 549 1000 601 1000 659 824 687 795 601 769 601 601 769 769 713 250 713 713 713 713 713 769 713 791 791 891 824 549 601 713 604 604 1042 987 604 987 604 495 330 791 791 787 713 384 384 384 384 384 384 495 495 495 495 601 330 274 687 687 687 384 384 384 384 384 384 495 495 495 601 ] endobj 20 0 obj << /Type /FontDescriptor /Ascent 823 /CapHeight 0 /Descent -277 /Flags 32 /FontBBox [ -230 -483 1095 996 ] /FontName /RFNJXW+Palatino-Roman /ItalicAngle 0 /StemV 0 /MaxWidth 1144 /FontFile2 39 0 R >> endobj 21 0 obj << /Type /Font /Subtype /TrueType /BaseFont /HCHHXU+Symbol /FontDescriptor 18 0 R /Widths 19 0 R /FirstChar 0 /LastChar 255 /Encoding /MacRomanEncoding >> endobj 22 0 obj [ 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 500 152 245 262 497 459 568 468 147 308 264 402 833 156 270 137 318 485 262 388 405 403 457 431 379 454 392 173 162 833 833 833 405 585 496 509 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elastic rebound theoryTheory which holds that accumulated potential energy, stored as elastic strains, is released by faulting (i.e. x��W�r�H}���G��!�Aysmy/Y����*/����!3`��~� "�L�e@�g�O�9���'81��eǶAB�y����_(�ív �`����m����{�c��Q�C�ç�N����g�6,r��c���b W�=�{�0_�� H��"�ø:H���T��/��u~ �m�������ǧ�A�'����\�6K�VR�p[+%�:��a. 0000048235 00000 n In these subduction zones, friction causes the top plate to bend and store elastic energy. 0000049054 00000 n Such irregular properties of fault rupture are now included in the modeling of earthquake sources, both physically and mathematically. 0000001477 00000 n 10 0 obj << /Linearized 1 /O 12 /H [ 1477 249 ] /L 139390 /E 130839 /N 2 /T 139072 >> endobj xref 10 53 0000000016 00000 n The following diagram illustrates the process. - Definition & Location, Accretionary Wedge: Definition & Formation, Biological and Biomedical For more information, see the following related content on ScienceDaily: Content on this website is for information only. 0000002253 00000 n 0000011412 00000 n Reid, H.F., The Mechanics of the Earthquake, The California Start at the bottom. Elastic rebound, as demonstrated by a rubber band, is an important concept to understand when studying earthquakes and their effects. 0000005421 00000 n These observations provided the basis for the landmark "theory of elastic rebound", introduced by Professor H.F. Reid of Johns Hopkins University, who served on Lawson's Commission. In geology, the elastic rebound theory was the first theory to satisfactorily explain earthquakes. In dip-slip faults, if the hanging-wall block moves downward relative to the footwall block, it is called “normal” faulting; the opposite motion, with the hanging wall moving upward relative to the footwall, produces reverse or thrust faulting. It is estimated that only 10 percent or less of an earthquake's total energy is radiated as seismic energy. The usual fault model has a “strike” (that is, the direction from north taken by a horizontal line in the fault plane) and a “dip” (the angle from the horizontal shown by the steepest slope in the fault). The actual faulting associated with an earthquake may be complex, and it is often not clear whether in a particular earthquake the total energy issues from a single fault plane. Once there is a lot of elastic energy stored, you can let it go.

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