Genesis of the Early Indosinian Darongshan Granitoid in South China: Response to the Subduction of the Eastern Paleo-Tethys Ocean

<div>(a) Histogram of zircon <svg height="12.552pt" id="M37" style="vertical-align:-3.26367pt" version="1.1" viewbox="-0.0498162 -9.28833 29.0936 12.552" width="29.0936pt" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink"><g transform="matrix(.0091,0,0,-0.0091,0,3.132)"><path d="M389 366C309 366 253 375 222 392C183 413 164 445 164 490C164 578 219 638 327 638S510 566 525 449H548L538 676H518C513 654 500 643 480 643C473 643 449 649 409 661C372 671 337 676 304 676C145 676 62 604 62 501C62 464 76 431 104 403C135 372 174 354 219 349V348C151 344 98 327 58 279C38 256 28 227 28 192C28 119 61 64 128 26C175 -1 232 -14 301 -14C342 -14 386 -6 432 9C467 21 498 38 523 59C548 81 561 104 561 129C561 156 549 169 524 169C505 169 491 158 483 147C475 137 459 104 448 87C423 49 382 30 327 30C210 30 143 85 143 182C143 231 161 267 198 291C235 314 298 326 389 326V366Z"></path></g><g transform="matrix(.0091,0,0,-0.0091,5.442,3.132)"><path d="M729 650H468V622C546 615 554 610 554 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526V124C128 39 120 33 34 27V0H270C392 0 492 25 567 83C643 141 690 230 690 350C690 444 655 517 605 565C543 625 450 650 323 650H43ZM213 547C213 587 217 598 226 604C236 612 262 617 304 617C371 617 429 604 474 576C554 529 592 439 592 336C592 176 505 36 319 36C246 36 213 55 213 131V547Z"></path></g><g transform="matrix(.0091,0,0,-0.0091,13.728,3.132)"><path d="M861 0V28C774 35 771 41 768 147L759 509C756 612 762 614 851 622V650H681L449 149L221 650H57V622C148 613 153 609 144 479L130 271C123 166 117 123 111 88C104 46 85 34 26 28V0H259V28C192 35 169 42 167 90C166 130 166 173 170 256L185 541H187L411 7H431L675 555H679L683 147C683 41 680 35 598 28V0H861Z"></path></g><g transform="matrix(.0091,0,0,-0.0091,21.891,3.132)"><path d="M414 144C384 79 371 75 317 75H135L276 221C367 316 408 376 408 465C408 570 327 635 237 635C179 635 131 609 100 575L42 494L67 471C94 510 138 565 205 565C277 565 321 517 321 435C321 348 258 270 195 195C146 137 88 81 33 26V0H411C423 44 433 88 446 135L414 144Z"></path></g><g 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d="M275 270C275 450 212 609 64 710L45 686C145 604 203 442 203 270S147 -63 45 -147L64 -170C213 -68 275 89 275 270Z"></path></g></svg> values for the granitoid samples from the Darongshan pluton. Data sources are referenced in Table <a href="https://static.hindawi.com/articles/geofluids/volume-2024/2387180/figures/#supplementary-material-1">S3</a> and Table <a href="https://static.hindawi.com/articles/geofluids/volume-2024/2387180/figures/#supplementary-material-1">S6</a> of the Supplementary Materials.</div>

Geofluids

fig9

Figure 9

Figure 9: Genesis of the Early Indosinian Darongshan Granitoid in South China: Response to the Subduction of the Eastern Paleo-Tethys Ocean 