Geoscience ›› 2022, Vol. 36 ›› Issue (01): 295-306.DOI: 10.19657/j.geoscience.1000-8527.2021.069
• Petrology • Previous Articles Next Articles
CHENG Xianyu1(), TIAN Jian1, DUAN Xiaolong1, ZHAO Zenan2, REN Bangfang1, ZHANG Yong1
Received:
2020-08-16
Revised:
2021-05-21
Online:
2022-02-10
Published:
2022-03-08
CLC Number:
CHENG Xianyu, TIAN Jian, DUAN Xiaolong, ZHAO Zenan, REN Bangfang, ZHANG Yong. Late Silurian to Early Devonian Tectonic Evolution of Beishanyang: Constraints from Geochronology and Geochemistry of Intrusive Rocks in Southern Baiyunshan Ophiolitic Mélange Belt, Inner Mongolia[J]. Geoscience, 2022, 36(01): 295-306.
Fig.1 Temporal-spatial distribution of ophiolites in the Beishan orogenic belt (a)[21],geological map of Yueyashan (b)[20] and sampling location map (c)
Fig.2 Macroscopic and microscopic characteristics of the quartz diorite (a)(b) and granodiorite from the southern part of Baiyunshan Ophiolitic mélange belt (c)(d)
样品号及点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | ||||||
---|---|---|---|---|---|---|---|---|---|---|
Th | U | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | |||
TW3422.1 | 379 | 429 | 0.88 | 0.055 2±0.000 6 | 0.510 2±0.007 3 | 0.067 1±0.000 7 | 420±26 | 419±6 | 418±5 | |
TW3422.2 | 396 | 448 | 0.88 | 0.055 3±0.000 6 | 0.511 3±0.006 7 | 0.067 0±0.000 7 | 426±26 | 419±6 | 418±4 | |
TW3422.3 | 1 055 | 977 | 1.08 | 0.055 0±0.000 6 | 0.511 5±0.006 9 | 0.067 4±0.000 7 | 413±25 | 419±6 | 421±4 | |
TW3422.4 | 675 | 625 | 1.08 | 0.055 6±0.000 7 | 0.513 6±0.007 2 | 0.067 0±0.000 6 | 436±28 | 421±6 | 418±4 | |
TW3422.5 | 377 | 450 | 0.84 | 0.054 6±0.000 6 | 0.512 5±0.007 0 | 0.068 0±0.000 7 | 397±27 | 420±6 | 424±4 | |
TW3422.6 | 315 | 365 | 0.86 | 0.055 7±0.000 7 | 0.519 8±0.008 5 | 0.067 7±0.000 8 | 441±28 | 425±7 | 422±5 | |
TW3422.7 | 909 | 858 | 1.06 | 0.054 4±0.000 6 | 0.508 4±0.007 0 | 0.067 7±0.000 7 | 390±25 | 417±6 | 422±5 | |
TW3422.8 | 465 | 467 | 1.00 | 0.055 4±0.000 6 | 0.512 2±0.007 1 | 0.067 1±0.000 7 | 428±26 | 420±6 | 418±5 | |
TW3422.9 | 88 | 173 | 0.51 | 0.055 4±0.001 0 | 0.513 4±0.010 0 | 0.067 2±0.000 7 | 428±39 | 421±8 | 419±5 | |
TW3422.10 | 353 | 446 | 0.79 | 0.054 8±0.000 6 | 0.509 8±0.006 8 | 0.067 5±0.000 7 | 403±26 | 418±6 | 421±4 | |
TW3422.11 | 268 | 362 | 0.74 | 0.055 1±0.000 7 | 0.512 5±0.007 0 | 0.067 5±0.000 7 | 415±26 | 420±6 | 421±4 | |
TW3422.12 | 440 | 367 | 1.20 | 0.054 9±0.002 1 | 0.512 2±0.021 2 | 0.067 7±0.000 8 | 406±86 | 420±17 | 422±5 | |
TW3422.13 | 349 | 390 | 0.89 | 0.054 9±0.000 7 | 0.510 2±0.007 1 | 0.067 4±0.000 7 | 408±28 | 419±6 | 420±4 | |
TW3422.14 | 450 | 513 | 0.88 | 0.054 9±0.000 6 | 0.511 0±0.006 8 | 0.067 5±0.000 7 | 408±26 | 419±6 | 421±4 | |
TW3422.15 | 340 | 461 | 0.74 | 0.054 5±0.000 6 | 0.508 3±0.007 0 | 0.067 7±0.000 7 | 390±26 | 417±6 | 422±4 | |
TW3422.16 | 396 | 527 | 0.75 | 0.054 6±0.000 6 | 0.507 9±0.007 4 | 0.067 5±0.000 8 | 395±26 | 417±6 | 421±5 | |
TW3422.17 | 463 | 461 | 1.00 | 0.055 7±0.000 7 | 0.515 6±0.007 1 | 0.067 2±0.000 7 | 440±26 | 422±6 | 419±4 | |
TW3422.18 | 140 | 240 | 0.59 | 0.055 0±0.001 1 | 0.510 3±0.012 8 | 0.067 3±0.000 8 | 410±43 | 419±11 | 420±5 | |
TW3422.19 | 358 | 365 | 0.98 | 0.055 0±0.000 7 | 0.509 6±0.007 4 | 0.067 2±0.000 7 | 413±27 | 418±6 | 419±4 | |
TW3422.20 | 359 | 338 | 1.06 | 0.054 8±0.000 7 | 0.509 3±0.007 4 | 0.067 4±0.000 7 | 404±28 | 418±6 | 420±4 | |
TW3422.21 | 264 | 366 | 0.72 | 0.055 2±0.000 7 | 0.508 4±0.007 1 | 0.066 8±0.000 7 | 420±27 | 417±6 | 417±4 | |
TW3422.22 | 382 | 417 | 0.92 | 0.054 9±0.000 6 | 0.507 5±0.006 9 | 0.067 0±0.000 7 | 410±26 | 417±6 | 418±4 | |
TW3422.23 | 948 | 891 | 1.06 | 0.055 5±0.000 6 | 0.512 0±0.007 0 | 0.066 9±0.000 7 | 433±25 | 420±6 | 417±5 | |
TW3422.24 | 395 | 528 | 0.75 | 0.055 5±0.000 6 | 0.512 2±0.006 8 | 0.067 0±0.000 7 | 431±26 | 420±6 | 418±4 | |
TW3424-1.01 | 15 | 36 | 0.41 | 0.053 5±0.004 3 | 0.491 9±0.040 2 | 0.066 6±0.000 8 | 351±181 | 406±33 | 416±4 | |
TW3424-1.02 | 39 | 59 | 0.66 | 0.055 2±0.002 7 | 0.493 3±0.024 2 | 0.064 8±0.000 7 | 419±108 | 407±20 | 405±4 | |
TW3424-1.03 | 13 | 27 | 0.47 | 0.056 6±0.005 0 | 0.510 5±0.045 4 | 0.065 4±0.000 8 | 476±195 | 419±37 | 409±5 | |
TW3424-1.04 | 17 | 30 | 0.56 | 0.055 3±0.004 1 | 0.495 0±0.036 8 | 0.065 0±0.000 7 | 423±166 | 408±30 | 406±5 | |
TW3424-1.05 | 11 | 23 | 0.50 | 0.056 7±0.007 3 | 0.472 4±0.061 2 | 0.060 4±0.000 9 | 481±286 | 393±51 | 378±6 | |
TW3424-1.06 | 31 | 50 | 0.62 | 0.053 0±0.002 5 | 0.482 3±0.023 5 | 0.066 0±0.000 7 | 330±108 | 400±19 | 412±4 | |
TW3424-1.07 | 21 | 44 | 0.49 | 0.056 1±0.002 9 | 0.506 2±0.026 5 | 0.065 5±0.000 7 | 454±113 | 416±22 | 409±4 | |
TW3424-1.08 | 13 | 28 | 0.45 | 0.053 8±0.004 6 | 0.498 6±0.043 0 | 0.067 2±0.000 8 | 364±192 | 411±35 | 419±5 | |
TW3424-1.09 | 10 | 29 | 0.36 | 0.055 6±0.005 8 | 0.488 8±0.049 8 | 0.063 8±0.000 8 | 435±232 | 404±41 | 399±5 | |
TW3424-1.10 | 17 | 40 | 0.44 | 0.057 5±0.004 1 | 0.509 5±0.035 6 | 0.064 2±0.000 7 | 512±156 | 418±29 | 401±5 | |
TW3424-1.11 | 108 | 67 | 1.61 | 0.055 2±0.005 0 | 0.428 0±0.039 0 | 0.056 2±0.000 6 | 421±201 | 362±33 | 353±4 | |
TW3424-1.12 | 30 | 42 | 0.71 | 0.055 4±0.003 5 | 0.494 2±0.031 3 | 0.064 7±0.000 7 | 427±141 | 408±26 | 404±4 | |
样品号及点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | ||||||
Th | U | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | 206Pb/238U ±1σ | 207Pb/235U ±1σ | 207Pb/206Pb ±1σ | |||
TW3424-1.13 | 16 | 39 | 0.41 | 0.053 8±0.004 1 | 0.486 0±0.037 9 | 0.065 5±0.000 7 | 364±174 | 402±31 | 409±5 | |
TW3424-1.14 | 19 | 44 | 0.43 | 0.056 0±0.003 1 | 0.502 0±0.028 6 | 0.065 0±0.000 7 | 454±124 | 413±24 | 406±5 | |
TW3424-1.15 | 32 | 55 | 0.59 | 0.054 5±0.002 4 | 0.479 8±0.021 2 | 0.063 8±0.000 7 | 393±97 | 398±18 | 399±4 | |
TW3424-1.16 | 30 | 51 | 0.59 | 0.056 2±0.002 4 | 0.490 3±0.021 1 | 0.063 3±0.000 7 | 459±94 | 405±17 | 396±4 | |
TW3424-1.17 | 18 | 47 | 0.39 | 0.053 9±0.002 6 | 0.487 5±0.024 3 | 0.065 6±0.000 7 | 368±109 | 403±20 | 409±4 | |
TW3424-1.18 | 14 | 35 | 0.41 | 0.056 3±0.003 6 | 0.487 5±0.031 9 | 0.062 8±0.000 7 | 465±143 | 403±26 | 392±4 | |
TW3424-1.19 | 14 | 33 | 0.44 | 0.053 5±0.004 1 | 0.473 4±0.036 0 | 0.064 2±0.000 7 | 351±172 | 394±30 | 401±5 | |
TW3424-1.20 | 28 | 45 | 0.63 | 0.053 9±0.003 1 | 0.475 5±0.028 3 | 0.064 0±0.000 8 | 366±131 | 395±24 | 400±5 | |
TW3424-1.21 | 29 | 50 | 0.57 | 0.054 4±0.002 9 | 0.479 5±0.026 2 | 0.063 9±0.000 7 | 387±121 | 398±22 | 400±4 | |
TW3424-1.22 | 27 | 44 | 0.61 | 0.054 2±0.003 0 | 0.491 8±0.027 4 | 0.065 8±0.000 7 | 381±124 | 406±23 | 411±4 | |
TW3424-1.23 | 28 | 68 | 0.41 | 0.053 5±0.001 9 | 0.481 9±0.017 6 | 0.065 3±0.000 7 | 352±80 | 399±15 | 408±4 | |
TW3424-1.24 | 22 | 59 | 0.38 | 0.054 0±0.002 5 | 0.486 7±0.022 9 | 0.065 3±0.000 7 | 373±103 | 403±19 | 408±4 |
Table 1 Zircon LA-ICP-MS U-Pb dating results of the quartz diorite (TW3422) and granodiorite (TW3424-1)
样品号及点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | ||||||
---|---|---|---|---|---|---|---|---|---|---|
Th | U | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | |||
TW3422.1 | 379 | 429 | 0.88 | 0.055 2±0.000 6 | 0.510 2±0.007 3 | 0.067 1±0.000 7 | 420±26 | 419±6 | 418±5 | |
TW3422.2 | 396 | 448 | 0.88 | 0.055 3±0.000 6 | 0.511 3±0.006 7 | 0.067 0±0.000 7 | 426±26 | 419±6 | 418±4 | |
TW3422.3 | 1 055 | 977 | 1.08 | 0.055 0±0.000 6 | 0.511 5±0.006 9 | 0.067 4±0.000 7 | 413±25 | 419±6 | 421±4 | |
TW3422.4 | 675 | 625 | 1.08 | 0.055 6±0.000 7 | 0.513 6±0.007 2 | 0.067 0±0.000 6 | 436±28 | 421±6 | 418±4 | |
TW3422.5 | 377 | 450 | 0.84 | 0.054 6±0.000 6 | 0.512 5±0.007 0 | 0.068 0±0.000 7 | 397±27 | 420±6 | 424±4 | |
TW3422.6 | 315 | 365 | 0.86 | 0.055 7±0.000 7 | 0.519 8±0.008 5 | 0.067 7±0.000 8 | 441±28 | 425±7 | 422±5 | |
TW3422.7 | 909 | 858 | 1.06 | 0.054 4±0.000 6 | 0.508 4±0.007 0 | 0.067 7±0.000 7 | 390±25 | 417±6 | 422±5 | |
TW3422.8 | 465 | 467 | 1.00 | 0.055 4±0.000 6 | 0.512 2±0.007 1 | 0.067 1±0.000 7 | 428±26 | 420±6 | 418±5 | |
TW3422.9 | 88 | 173 | 0.51 | 0.055 4±0.001 0 | 0.513 4±0.010 0 | 0.067 2±0.000 7 | 428±39 | 421±8 | 419±5 | |
TW3422.10 | 353 | 446 | 0.79 | 0.054 8±0.000 6 | 0.509 8±0.006 8 | 0.067 5±0.000 7 | 403±26 | 418±6 | 421±4 | |
TW3422.11 | 268 | 362 | 0.74 | 0.055 1±0.000 7 | 0.512 5±0.007 0 | 0.067 5±0.000 7 | 415±26 | 420±6 | 421±4 | |
TW3422.12 | 440 | 367 | 1.20 | 0.054 9±0.002 1 | 0.512 2±0.021 2 | 0.067 7±0.000 8 | 406±86 | 420±17 | 422±5 | |
TW3422.13 | 349 | 390 | 0.89 | 0.054 9±0.000 7 | 0.510 2±0.007 1 | 0.067 4±0.000 7 | 408±28 | 419±6 | 420±4 | |
TW3422.14 | 450 | 513 | 0.88 | 0.054 9±0.000 6 | 0.511 0±0.006 8 | 0.067 5±0.000 7 | 408±26 | 419±6 | 421±4 | |
TW3422.15 | 340 | 461 | 0.74 | 0.054 5±0.000 6 | 0.508 3±0.007 0 | 0.067 7±0.000 7 | 390±26 | 417±6 | 422±4 | |
TW3422.16 | 396 | 527 | 0.75 | 0.054 6±0.000 6 | 0.507 9±0.007 4 | 0.067 5±0.000 8 | 395±26 | 417±6 | 421±5 | |
TW3422.17 | 463 | 461 | 1.00 | 0.055 7±0.000 7 | 0.515 6±0.007 1 | 0.067 2±0.000 7 | 440±26 | 422±6 | 419±4 | |
TW3422.18 | 140 | 240 | 0.59 | 0.055 0±0.001 1 | 0.510 3±0.012 8 | 0.067 3±0.000 8 | 410±43 | 419±11 | 420±5 | |
TW3422.19 | 358 | 365 | 0.98 | 0.055 0±0.000 7 | 0.509 6±0.007 4 | 0.067 2±0.000 7 | 413±27 | 418±6 | 419±4 | |
TW3422.20 | 359 | 338 | 1.06 | 0.054 8±0.000 7 | 0.509 3±0.007 4 | 0.067 4±0.000 7 | 404±28 | 418±6 | 420±4 | |
TW3422.21 | 264 | 366 | 0.72 | 0.055 2±0.000 7 | 0.508 4±0.007 1 | 0.066 8±0.000 7 | 420±27 | 417±6 | 417±4 | |
TW3422.22 | 382 | 417 | 0.92 | 0.054 9±0.000 6 | 0.507 5±0.006 9 | 0.067 0±0.000 7 | 410±26 | 417±6 | 418±4 | |
TW3422.23 | 948 | 891 | 1.06 | 0.055 5±0.000 6 | 0.512 0±0.007 0 | 0.066 9±0.000 7 | 433±25 | 420±6 | 417±5 | |
TW3422.24 | 395 | 528 | 0.75 | 0.055 5±0.000 6 | 0.512 2±0.006 8 | 0.067 0±0.000 7 | 431±26 | 420±6 | 418±4 | |
TW3424-1.01 | 15 | 36 | 0.41 | 0.053 5±0.004 3 | 0.491 9±0.040 2 | 0.066 6±0.000 8 | 351±181 | 406±33 | 416±4 | |
TW3424-1.02 | 39 | 59 | 0.66 | 0.055 2±0.002 7 | 0.493 3±0.024 2 | 0.064 8±0.000 7 | 419±108 | 407±20 | 405±4 | |
TW3424-1.03 | 13 | 27 | 0.47 | 0.056 6±0.005 0 | 0.510 5±0.045 4 | 0.065 4±0.000 8 | 476±195 | 419±37 | 409±5 | |
TW3424-1.04 | 17 | 30 | 0.56 | 0.055 3±0.004 1 | 0.495 0±0.036 8 | 0.065 0±0.000 7 | 423±166 | 408±30 | 406±5 | |
TW3424-1.05 | 11 | 23 | 0.50 | 0.056 7±0.007 3 | 0.472 4±0.061 2 | 0.060 4±0.000 9 | 481±286 | 393±51 | 378±6 | |
TW3424-1.06 | 31 | 50 | 0.62 | 0.053 0±0.002 5 | 0.482 3±0.023 5 | 0.066 0±0.000 7 | 330±108 | 400±19 | 412±4 | |
TW3424-1.07 | 21 | 44 | 0.49 | 0.056 1±0.002 9 | 0.506 2±0.026 5 | 0.065 5±0.000 7 | 454±113 | 416±22 | 409±4 | |
TW3424-1.08 | 13 | 28 | 0.45 | 0.053 8±0.004 6 | 0.498 6±0.043 0 | 0.067 2±0.000 8 | 364±192 | 411±35 | 419±5 | |
TW3424-1.09 | 10 | 29 | 0.36 | 0.055 6±0.005 8 | 0.488 8±0.049 8 | 0.063 8±0.000 8 | 435±232 | 404±41 | 399±5 | |
TW3424-1.10 | 17 | 40 | 0.44 | 0.057 5±0.004 1 | 0.509 5±0.035 6 | 0.064 2±0.000 7 | 512±156 | 418±29 | 401±5 | |
TW3424-1.11 | 108 | 67 | 1.61 | 0.055 2±0.005 0 | 0.428 0±0.039 0 | 0.056 2±0.000 6 | 421±201 | 362±33 | 353±4 | |
TW3424-1.12 | 30 | 42 | 0.71 | 0.055 4±0.003 5 | 0.494 2±0.031 3 | 0.064 7±0.000 7 | 427±141 | 408±26 | 404±4 | |
样品号及点号 | 含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | ||||||
Th | U | 207Pb/206Pb ±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | 206Pb/238U ±1σ | 207Pb/235U ±1σ | 207Pb/206Pb ±1σ | |||
TW3424-1.13 | 16 | 39 | 0.41 | 0.053 8±0.004 1 | 0.486 0±0.037 9 | 0.065 5±0.000 7 | 364±174 | 402±31 | 409±5 | |
TW3424-1.14 | 19 | 44 | 0.43 | 0.056 0±0.003 1 | 0.502 0±0.028 6 | 0.065 0±0.000 7 | 454±124 | 413±24 | 406±5 | |
TW3424-1.15 | 32 | 55 | 0.59 | 0.054 5±0.002 4 | 0.479 8±0.021 2 | 0.063 8±0.000 7 | 393±97 | 398±18 | 399±4 | |
TW3424-1.16 | 30 | 51 | 0.59 | 0.056 2±0.002 4 | 0.490 3±0.021 1 | 0.063 3±0.000 7 | 459±94 | 405±17 | 396±4 | |
TW3424-1.17 | 18 | 47 | 0.39 | 0.053 9±0.002 6 | 0.487 5±0.024 3 | 0.065 6±0.000 7 | 368±109 | 403±20 | 409±4 | |
TW3424-1.18 | 14 | 35 | 0.41 | 0.056 3±0.003 6 | 0.487 5±0.031 9 | 0.062 8±0.000 7 | 465±143 | 403±26 | 392±4 | |
TW3424-1.19 | 14 | 33 | 0.44 | 0.053 5±0.004 1 | 0.473 4±0.036 0 | 0.064 2±0.000 7 | 351±172 | 394±30 | 401±5 | |
TW3424-1.20 | 28 | 45 | 0.63 | 0.053 9±0.003 1 | 0.475 5±0.028 3 | 0.064 0±0.000 8 | 366±131 | 395±24 | 400±5 | |
TW3424-1.21 | 29 | 50 | 0.57 | 0.054 4±0.002 9 | 0.479 5±0.026 2 | 0.063 9±0.000 7 | 387±121 | 398±22 | 400±4 | |
TW3424-1.22 | 27 | 44 | 0.61 | 0.054 2±0.003 0 | 0.491 8±0.027 4 | 0.065 8±0.000 7 | 381±124 | 406±23 | 411±4 | |
TW3424-1.23 | 28 | 68 | 0.41 | 0.053 5±0.001 9 | 0.481 9±0.017 6 | 0.065 3±0.000 7 | 352±80 | 399±15 | 408±4 | |
TW3424-1.24 | 22 | 59 | 0.38 | 0.054 0±0.002 5 | 0.486 7±0.022 9 | 0.065 3±0.000 7 | 373±103 | 403±19 | 408±4 |
Fig.3 Cathodoluminescence images and U-Pb concordia diagrams for zircons from the quartz diorite (a)(c) and granodiorite (b)(d) in the southern part of the Baiyunshan ophiolitic mélange belt
样品号 | 岩性 | SiO2 | Al2O3 | Fe2O3 | FeO | CaO | MgO | K2O | Na2O | TiO2 | P2O5 | MnO | 烧失量 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
YQ3422-1 | 石英闪长岩 | 58.46 | 16.83 | 1.82 | 4.36 | 5.74 | 3.33 | 1.38 | 4.15 | 1.29 | 0.23 | 0.11 | 1.81 |
YQ3422-2 | 石英闪长岩 | 58.38 | 16.95 | 2.05 | 4.52 | 5.41 | 3.21 | 1.31 | 4.34 | 1.21 | 0.24 | 0.12 | 1.78 |
YQ3424-1 | 花岗闪长岩 | 69.20 | 15.72 | 1.30 | 1.20 | 2.66 | 1.59 | 0.74 | 5.36 | 0.32 | 0.08 | 0.06 | 1.64 |
YQ3424-2 | 花岗闪长岩 | 69.46 | 15.54 | 1.04 | 1.31 | 2.76 | 1.50 | 0.84 | 5.32 | 0.34 | 0.08 | 0.04 | 1.62 |
样品号 | 岩性 | 总量 | Na2O+K2O | Na2O/K2O | Cu | Pb | Zn | Cr | Ni | Co | Li | Rb | Cs |
YQ3422-1 | 石英闪长岩 | 99.51 | 5.53 | 3.01 | 12.90 | 7.10 | 57.8 | 34.7 | 16.00 | 20.50 | 20.20 | 33.1 | 1.55 |
YQ3422-2 | 石英闪长岩 | 99.52 | 5.65 | 3.31 | 24.90 | 7.74 | 75.7 | 29.1 | 13.90 | 20.50 | 14.40 | 40.3 | 1.88 |
YQ3424-1 | 花岗闪长岩 | 99.87 | 6.10 | 7.24 | 2.87 | 3.90 | 27.0 | 19.5 | 9.26 | 6.62 | 5.87 | 23.3 | 3.20 |
YQ3424-2 | 花岗闪长岩 | 99.85 | 6.16 | 6.33 | 3.11 | 3.72 | 26.6 | 18.1 | 8.81 | 6.42 | 5.23 | 29.8 | 2.82 |
样品号 | 岩性 | Bi | Sr | Ba | V | Sc | Y | Nb | Ta | Zr | Hf | Be | Ga |
YQ3422-1 | 石英闪长岩 | 0.028 | 301 | 278 | 129.0 | 16.60 | 28.50 | 7.29 | 0.68 | 205 | 5.86 | 1.51 | 19.1 |
YQ3422-2 | 石英闪长岩 | 0.027 | 304 | 297 | 137.0 | 14.80 | 26.90 | 6.13 | 0.58 | 114 | 3.58 | 1.52 | 19.0 |
YQ3424-1 | 花岗闪长岩 | 0.015 | 303 | 99 | 32.9 | 2.25 | 7.47 | 2.27 | 0.21 | 159 | 4.05 | 0.84 | 13.4 |
YQ3424-2 | 花岗闪长岩 | 0.016 | 276 | 123 | 33.5 | 2.36 | 7.46 | 2.39 | 0.22 | 128 | 3.81 | 1.00 | 13.3 |
样品号 | 岩性 | U | Th | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho |
YQ3422-1 | 石英闪长岩 | 1.15 | 4.87 | 17.00 | 36.3 | 5.10 | 22.00 | 5.20 | 1.36 | 5.90 | 0.97 | 5.78 | 1.12 |
YQ3422-2 | 石英闪长岩 | 0.91 | 3.89 | 15.80 | 32.9 | 4.72 | 20.50 | 4.97 | 1.47 | 5.53 | 0.90 | 5.39 | 1.05 |
YQ3424-1 | 花岗闪长岩 | 0.51 | 1.78 | 6.30 | 14.2 | 1.83 | 7.54 | 1.73 | 0.50 | 1.79 | 0.28 | 1.51 | 0.30 |
YQ3424-2 | 花岗闪长岩 | 0.58 | 2.01 | 6.29 | 13.3 | 1.75 | 7.10 | 1.59 | 0.52 | 1.72 | 0.26 | 1.52 | 0.28 |
样品号 | 岩性 | Er | Tm | Yb | Lu | REE | LREE | HREE | LREE/HREE | δEu | δCe | (La/Yb)N | |
YQ3422-1 | 石英闪长岩 | 3.04 | 0.43 | 2.95 | 0.45 | 107.6 | 86.96 | 20.64 | 4.21 | 0.75 | 0.96 | 4.13 | |
YQ3422-2 | 石英闪长岩 | 2.81 | 0.40 | 2.69 | 0.40 | 99.53 | 80.36 | 19.17 | 4.19 | 0.86 | 0.93 | 4.21 | |
YQ3424-1 | 花岗闪长岩 | 0.74 | 0.11 | 0.70 | 0.11 | 37.64 | 32.10 | 5.54 | 5.79 | 0.87 | 1.03 | 6.46 | |
YQ3424-2 | 花岗闪长岩 | 0.74 | 0.11 | 0.75 | 0.11 | 36.04 | 30.55 | 5.49 | 5.56 | 0.96 | 0.98 | 6.02 |
Table 2 Major element (%), trace element (10-6), and rare earth element (10-6) compositions of intermediate-felsic dyke samples
样品号 | 岩性 | SiO2 | Al2O3 | Fe2O3 | FeO | CaO | MgO | K2O | Na2O | TiO2 | P2O5 | MnO | 烧失量 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
YQ3422-1 | 石英闪长岩 | 58.46 | 16.83 | 1.82 | 4.36 | 5.74 | 3.33 | 1.38 | 4.15 | 1.29 | 0.23 | 0.11 | 1.81 |
YQ3422-2 | 石英闪长岩 | 58.38 | 16.95 | 2.05 | 4.52 | 5.41 | 3.21 | 1.31 | 4.34 | 1.21 | 0.24 | 0.12 | 1.78 |
YQ3424-1 | 花岗闪长岩 | 69.20 | 15.72 | 1.30 | 1.20 | 2.66 | 1.59 | 0.74 | 5.36 | 0.32 | 0.08 | 0.06 | 1.64 |
YQ3424-2 | 花岗闪长岩 | 69.46 | 15.54 | 1.04 | 1.31 | 2.76 | 1.50 | 0.84 | 5.32 | 0.34 | 0.08 | 0.04 | 1.62 |
样品号 | 岩性 | 总量 | Na2O+K2O | Na2O/K2O | Cu | Pb | Zn | Cr | Ni | Co | Li | Rb | Cs |
YQ3422-1 | 石英闪长岩 | 99.51 | 5.53 | 3.01 | 12.90 | 7.10 | 57.8 | 34.7 | 16.00 | 20.50 | 20.20 | 33.1 | 1.55 |
YQ3422-2 | 石英闪长岩 | 99.52 | 5.65 | 3.31 | 24.90 | 7.74 | 75.7 | 29.1 | 13.90 | 20.50 | 14.40 | 40.3 | 1.88 |
YQ3424-1 | 花岗闪长岩 | 99.87 | 6.10 | 7.24 | 2.87 | 3.90 | 27.0 | 19.5 | 9.26 | 6.62 | 5.87 | 23.3 | 3.20 |
YQ3424-2 | 花岗闪长岩 | 99.85 | 6.16 | 6.33 | 3.11 | 3.72 | 26.6 | 18.1 | 8.81 | 6.42 | 5.23 | 29.8 | 2.82 |
样品号 | 岩性 | Bi | Sr | Ba | V | Sc | Y | Nb | Ta | Zr | Hf | Be | Ga |
YQ3422-1 | 石英闪长岩 | 0.028 | 301 | 278 | 129.0 | 16.60 | 28.50 | 7.29 | 0.68 | 205 | 5.86 | 1.51 | 19.1 |
YQ3422-2 | 石英闪长岩 | 0.027 | 304 | 297 | 137.0 | 14.80 | 26.90 | 6.13 | 0.58 | 114 | 3.58 | 1.52 | 19.0 |
YQ3424-1 | 花岗闪长岩 | 0.015 | 303 | 99 | 32.9 | 2.25 | 7.47 | 2.27 | 0.21 | 159 | 4.05 | 0.84 | 13.4 |
YQ3424-2 | 花岗闪长岩 | 0.016 | 276 | 123 | 33.5 | 2.36 | 7.46 | 2.39 | 0.22 | 128 | 3.81 | 1.00 | 13.3 |
样品号 | 岩性 | U | Th | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho |
YQ3422-1 | 石英闪长岩 | 1.15 | 4.87 | 17.00 | 36.3 | 5.10 | 22.00 | 5.20 | 1.36 | 5.90 | 0.97 | 5.78 | 1.12 |
YQ3422-2 | 石英闪长岩 | 0.91 | 3.89 | 15.80 | 32.9 | 4.72 | 20.50 | 4.97 | 1.47 | 5.53 | 0.90 | 5.39 | 1.05 |
YQ3424-1 | 花岗闪长岩 | 0.51 | 1.78 | 6.30 | 14.2 | 1.83 | 7.54 | 1.73 | 0.50 | 1.79 | 0.28 | 1.51 | 0.30 |
YQ3424-2 | 花岗闪长岩 | 0.58 | 2.01 | 6.29 | 13.3 | 1.75 | 7.10 | 1.59 | 0.52 | 1.72 | 0.26 | 1.52 | 0.28 |
样品号 | 岩性 | Er | Tm | Yb | Lu | REE | LREE | HREE | LREE/HREE | δEu | δCe | (La/Yb)N | |
YQ3422-1 | 石英闪长岩 | 3.04 | 0.43 | 2.95 | 0.45 | 107.6 | 86.96 | 20.64 | 4.21 | 0.75 | 0.96 | 4.13 | |
YQ3422-2 | 石英闪长岩 | 2.81 | 0.40 | 2.69 | 0.40 | 99.53 | 80.36 | 19.17 | 4.19 | 0.86 | 0.93 | 4.21 | |
YQ3424-1 | 花岗闪长岩 | 0.74 | 0.11 | 0.70 | 0.11 | 37.64 | 32.10 | 5.54 | 5.79 | 0.87 | 1.03 | 6.46 | |
YQ3424-2 | 花岗闪长岩 | 0.74 | 0.11 | 0.75 | 0.11 | 36.04 | 30.55 | 5.49 | 5.56 | 0.96 | 0.98 | 6.02 |
Fig.5 A/CNK-A/NK diagram for the granodiorite (a)) and granite-type discrimination diagrams (b)(c)(d) for the southern part of the Baiyunshan ophiolitic mélange belt (base map after ref.[29])
Fig.6 Chondrite-normalized REE patterns (a) and primitive mantle-normalized multi-element patterns (b) for the intermediate-felsic intrusive rocks in the southern part of the Baiyunshan ophiolitic mélange belt (base map after ref.[30])
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