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

<div>(a) <svg height="12.599pt" id="M52" style="vertical-align:-3.2911pt" version="1.1" viewbox="-0.0498162 -9.3079 50.6318 12.599" width="50.6318pt" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink"><g transform="matrix(.013,0,0,-0.013,0,0)"><path d="M300 -147C201 -63 143 98 143 270S200 602 300 686L282 710C136 610 70 450 70 271V270C70 89 136 -72 282 -170L300 -147Z"></path></g><g transform="matrix(.013,0,0,-0.013,4.498,0)"><path d="M495 163C480 117 462 85 444 65C421 39 387 34 332 34C290 34 256 36 236 47C218 57 213 77 213 131V526C213 612 222 616 301 622V650H40V622C122 616 128 611 128 526V126C128 41 120 34 36 28V0H489C498 31 519 126 525 157L495 163Z"></path></g><g transform="matrix(.013,0,0,-0.013,11.688,0)"><path d="M433 39L423 65C413 59 399 54 387 54C370 54 352 69 352 114V299C352 352 342 392 307 422C285 440 255 449 225 449C168 437 102 399 75 379C56 365 44 353 44 339C44 315 69 296 87 296C101 296 111 303 116 319C124 349 133 371 145 385C156 397 171 404 190 404C241 404 275 364 275 291V274C253 256 180 229 120 209C65 190 39 159 39 110C39 47 88 -12 159 -12C189 -12 237 25 277 52C282 35 288 21 301 8C312 -3 333 -12 348 -12L433 39ZM275 84C256 65 221 48 195 48C164 48 124 73 124 124C124 161 146 180 185 198C206 208 254 229 275 240V84Z"></path></g><g transform="matrix(.013,0,0,-0.013,17.442,0)"><path d="M368 703H309L44 -163H104L368 703Z"></path></g><g transform="matrix(.013,0,0,-0.013,22.804,0)"><path d="M620 650H399V622C477 614 480 606 457 556C429 495 375 397 338 331C295 406 246 488 203 568C185 601 182 613 254 622V650H15V622C75 617 86 606 126 537C180 445 217 379 252 318C269 287 273 278 273 258V125C273 40 265 34 176 28V0H458V28C366 34 358 41 358 125V261C358 287 361 298 375 324C422 412 456 470 501 543C539 604 551 614 620 622V650Z"></path></g><g transform="matrix(.013,0,0,-0.013,31.046,0)"><path d="M152 404V712C115 698 54 683 7 677V654C71 648 73 642 73 579V24C128 -2 179 -12 220 -12C353 -12 471 92 471 238C471 357 381 449 274 449C262 449 249 446 233 439L152 404ZM152 374C170 384 202 393 230 393C313 393 382 326 382 213C382 97 330 26 246 26C194 26 165 62 158 81C154 91 152 101 152 116V374Z"></path></g><g transform="matrix(.013,0,0,-0.013,37.705,0)"><path 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><g transform="matrix(.0091,0,0,-0.0091,42.203,3.132)"><path d="M870 650H622L613 619C694 615 708 606 708 559C708 531 702 477 686 396L636 136H633L281 650H127L120 619C180 616 198 611 212 592C227 572 232 558 220 503L166 254C148 169 139 131 126 89C112 43 85 35 33 32L24 0H280L286 32C208 37 189 44 189 93C189 124 198 179 212 250L267 526H271L622 -8H655L732 396C747 477 762 532 770 556C785 600 798 616 862 619L870 650Z"></path></g></svg> vs. <svg height="12.599pt" id="M53" style="vertical-align:-3.2911pt" version="1.1" viewbox="-0.0498162 -9.3079 23.2817 12.599" width="23.2817pt" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink"><g transform="matrix(.013,0,0,-0.013,0,0)"><path d="M620 650H399V622C477 614 480 606 457 556C429 495 375 397 338 331C295 406 246 488 203 568C185 601 182 613 254 622V650H15V622C75 617 86 606 126 537C180 445 217 379 252 318C269 287 273 278 273 258V125C273 40 265 34 176 28V0H458V28C366 34 358 41 358 125V261C358 287 361 298 375 324C422 412 456 470 501 543C539 604 551 614 620 622V650Z"></path></g><g transform="matrix(.013,0,0,-0.013,8.273,0)"><path d="M152 404V712C115 698 54 683 7 677V654C71 648 73 642 73 579V24C128 -2 179 -12 220 -12C353 -12 471 92 471 238C471 357 381 449 274 449C262 449 249 446 233 439L152 404ZM152 374C170 384 202 393 230 393C313 393 382 326 382 213C382 97 330 26 246 26C194 26 165 62 158 81C154 91 152 101 152 116V374Z"></path></g><g transform="matrix(.0091,0,0,-0.0091,14.902,3.132)"><path d="M870 650H622L613 619C694 615 708 606 708 559C708 531 702 477 686 396L636 136H633L281 650H127L120 619C180 616 198 611 212 592C227 572 232 558 220 503L166 254C148 169 139 131 126 89C112 43 85 35 33 32L24 0H280L286 32C208 37 189 44 189 93C189 124 198 179 212 250L267 526H271L622 -8H655L732 396C747 477 762 532 770 556C785 600 798 616 862 619L870 650Z"></path></g></svg> diagram (after [<a href="/journals/geofluids/2024/2387180/#B58">58</a>]). (b, c) SiO<sub>2</sub> vs. MgO and FeO<sup>T</sup>/MgO diagrams (simplified after [<a href="/journals/geofluids/2024/2387180/#B64">64</a>, <a href="/journals/geofluids/2024/2387180/#B68">68</a>]). HMA: high-Mg-andesitic/dioritic rocks; MA: Mg-andesitic/dioritic rocks; A: lower (or non)-Mg-andesitic/dioritic rocks; CA: calc-alkaline; TH: tholeiitic; LF-CA: low Fe-calc-alkaline. Legend is shown in Figure <a href="../fig6/">6</a>.</div>

Geofluids

fig11

Figure 11

Figure 11: Genesis of the Early Indosinian Darongshan Granitoid in South China: Response to the Subduction of the Eastern Paleo-Tethys Ocean 