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Table 1 References and descriptions for Fig. 2

From: Tectonic exhumation of a metamorphic core in an arc-continent collision during oblique convergence, Taiwan

 

References

Description

(A)

Yeh et al. (2016)

Black great circle and arrow show mean orientation of ductile shear zones and mean slip direction of hanging wall, respectively. N = 15. Site is on the RYUK block and is inferred to have rotated ~50° CW

(B)

Korren et al. (2017)

Black great circle and arrow show mean orientation faults lined with pseudotachylite and mean slip direction of hanging wall, respectively N = 21. Site is on the RYUK block and is inferred to have rotated ~50° CW

(C)

Lee (1995), Lee and Yang (1994)

Black great circle: mean orientation of late fold axial surfaces from 10 sites along Central Cross-Island Highway (CXIH) and the Tailuko coastline. Black dots: poles to F3 fold axial surfaces. N = 66. Black arrows: stretching direction from quartz veins. N = 100

(D) (D’)

Crespi et al. (1996)

Black arrows: extension direction interpreted from late-stage normal faults along the CXIH and SXIH

(E)

Ho and Lo (2015)

Black great circle: mean orientation of S3 from 3 domains along the Shoufeng River. N = 83

(F)

Yi et al. (2015)

Black arrow shows antiformal structure formed by S3 in the Yuli Belt

(G)

Lin (1999a, b), Yen (1970), Lin and Chen (2016)

Short dashed lines: intraformational strike-slip faults. Left-lateral faults from Lin (1999a; b) and Lin and Chen (2016). Right-lateral strike-slip fault from Yen (1970)

(H)

Clark et al. (1992)

Black great circles: mean orientation of S3 from 2 domains along the South Cross-Island Highway (SXIH). N = 276

(I)

Mondro et al. (2017)

Poles to composite foliation, Sc, and stretching lineation Lc, from Chulai and Hsinkao Formations (area in box). N = 46 and N = 40, respectively

(J)

Huang et al. (2014)

Regional-scale, late-stage antiform that deforms tectonic cleavage

(K)

Conand et al. (2020)

Poles to foliation, S1, and stretching lineation, L1, from sedimentary rocks south of southern most exposures of the Yuli Belt (area in box). N = 240 and N = 59, respectively

(L)

Fuller et al. (2006)

Apatite fission track ages of totally reset detrital grains; pooled ages

(M)

Lee et al. (2022a, b)

Major out-of-sequence thrust that carries the metamorphic core

(N)

Usami and Matsumoto (1940)

Late-stage left-lateral strike-slip faults on east and west sides of Tailuko Belt