In the original article, there was a mistake in Table 2 as published. In the “Reference” column, “Combined analysis with results from Li et al. (2016),” the citation should be Li Z. et al. (2017) instead of Li et al. (2016). The corrected Table 2 appears below.
TABLE 2
| ID | Formation/lithology | Location | Age (Ma) | Slat (°N) | Slong (°E) | N (n) | Plat (°N) | Plong (°E) | A95 (dp/dm)(°) | Paleolat (°N) | Field test | Reference |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Cretaceous paleopoles for the Lhasa Terrane (29.5°N, 91.0°E) | ||||||||||||
| TKR1 | Takena Fm. red beds | Linzhou | K2, 83 ± 17 | 29.9 | 91.2 | 7 (68) | 68 | 340 | 6.7/11.6 | 19.9 ± 6.7 | F, D | Pozzi et al. (1982) |
| TKR2 | Takena Fm. red beds | Linzhou | K2, 83 ± 17 | 29.9 | 91.2 | 6 (57) | 64 | 348 | 5.6/9.5 | 20.9 ± 5.6 | F | Westphal et al. (1983) |
| SXV | Shexing Fm. volcanic rocks | Linzhou | K2, 83 ± 17 | 29.9 | 91.2 | 21 (132) | 69.1 | 191.7 | 3.3/5.4 | 23.7 ± 3.3 | F | Tan et al. (2010) |
| SXR1 | Shexing Fm. red beds | Linzhou | K2, 83 ± 17 | 29.9 | 91.2 | 43 (377) | 70.2 | 300.5 | 1.4/2.7 | 11.9 ± 1.4 | F, D | Tan et al. (2010) |
| WRG | Woronggou Fm. volcanic rocks | Deqing | K1, ∼114 | 30.5 | 90.1 | 15 (88) | 66.4 | 220.3 | 6.9 | 13.3 ± 6.9 | no | Sun et al. (2008) |
| SXR2 | Shexing Fm. red beds | Maxiang | K2, 83 ± 17 | 29.9 | 90.7 | 17 (111) | 71.9 | 327.2 | 4.5 | 18.5 ± 4.5 | F | Sun et al. (2012) |
| TKR3 | Takena Fm. red beds | Barda | K2, 83 ± 17 | 31.7 | 91.5 | 6 (49) | 63.5 | 325.4 | 6.5 | 12.4 ± 6.5 | F | Achache et al. (1984) |
| TKR4 | Takena Fm. red beds | Linzhou | K2, 83 ± 17 | 29.9 | 91.1 | 8 (61) | 71.2 | 288.4 | 7.9 | 11.4 ± 7.9 | F | Achache et al. (1984) |
| ZC | Zenong Gp volcanic rocks | Cuoqen | 120 ± 10 | 31.3 | 85 | 18 | 58.2 | 341.9 | 4.6 | 15.6 ± 4.6 | F, R | Chen et al. (2012) |
| DJ | Duoai Fm. lava flow and Jiega Fm. limestone | Zuozuo | 114.5 ± 1.5 | 32.22 | 80.43 | 19 | 69.1 | 319.8 | 4.8 | 14.8 ± 4.8 | F, R | Bian et al. (2017) |
| LZZ | Linzizong Gp volcanic rocks | Cuoqen | 96 ± 3 | 30.6 | 85.2 | 10 (82) | 65.2 | 222.3 | 5.1 | 11.9 ± 5.1 | F | Tang et al. (2013) |
| QS | Qushenla Fm./lava flows | Yanhu | 126 ± 6 | 32.3 | 82.6 | 51 (444) | 61.4 | 192.9 | 2.1 | 20.3 ± 2.1 | F, D | Ma et al. (2014) |
| DN | Duoni Fm. volcanic rocks and redbeds | Nagqv | 120.2 ± 0.5 | 31.3 | 91.9 | 19 (139) | 66.9 | 281.2 | 6.1 | 6.7 ± 6.1 | F, D | Li Z. et al. (2017) |
| ZG | Zonggei Fm./volcanic rocks | Nagqv | 112 ± 2 | 31.48 | 92.1 | 9 (59) | 72.0 | 252.6 | 6.7 | 12.3 ± 6.7 | no | This study |
| ZG+DN | Zonggei and Duoni formations/volcanics + sediments | Nagqv | 115 ± 5 | 31.48 | 92.1 | 20 (144) | 70.3 | 270.5 | 5.2 | 9.8 ± 5.2 | F, D | Combined analysis with results from Li Z. et al. (2017) |
| TK5 | Takena Fm. red-beds | Linzhou | K2, 83 ± 17 | 29.9 | 91.2 | 8 (51) | 68 | 279 | 3.5/6.9 | 7.7 ± 3.5 | F | Lin and Watts (1988) |
| JZS | Jingzhushan Fm. red-beds | Dingqing | K2, 83 ± 17 | 31.22 | 95.98 | 15 (150) | 71.4 | 273.1 | 5.2 | 10.9 ± 5.2 | F | Tong, et al. (2017) |
| LR | Lava flow and red beds | Linzhou | 71.5 ± 3.5 | 29.9 | 91.1 | 21 (164) | 70.5 | 269.6 | 4.9 | 10.0 ± 4.9 | F, R | Cao et al. (2017) |
| SV | Volcanic rocks | Shiquanhe | 92.4 ± 0.9 | 32.34 | 80.03 | 10 (78) | 64.1 | 209 | 9.6 | 15.3 ± 9.6 | F, R | Yi et al. (2015) |
| CLC | Chalicuo Gp, volcanic rocks | Ya're | 79.6 ± 0.7 | 31.56 | 82.24 | 15 (136) | 68.4 | 298.8 | 2.7 | 10.0 ± 2.7 | F | Yi et al. (2015) |
| JZSC | Upper Cretaceous Jingzhushan Fm. sediments | Cuoqin | K2, 83 ± 17 | 31.13 | 84.86 | 33 | 63.5 | 324.9 | 2.1/3.9 | 12.2 ± 2.1 | F | Yang et al. (2015) |
| DZC | Dianzhong Fm., volcanics | Cuoqin | 119.0 ± 2.0 | 31.12 | 84.38 | 12 | 70.5 | 292.9 | 7.4 | 11.2 ± 7.4 | F | Yang et al. (2015) |
| Pre-Cretaceous paleopoles for the Lhasa Terrane (29.5°N, 91.0°E) | ||||||||||||
| SV | Sangri Gp, volcanic rocks | Sangri County | ∼180 Ma | 29.3 | 92.05 | 60 | 51.7 | 305.9 | 3.4 | −3.2 ± 3.4 | F, D | Li et al. (2016) |
| DCS1 | Dibu Co Lake, sediments | Coqin area | T1-2, 244.5 ± 7.5 Ma | 30.9 | 84.7 | 8 (25) | 16.6 | 204.6 | 5.6 | −11.1 ± 5.6 | F, R | Zhou et al. (2016) |
| DCS2 | Dibu Co Lake, sediments | Coqin area | T3, 219 ± 18 Ma | 30.9 | 84.7 | 6 (37) | 19.7 | 211 | 4.7 | −14.1 ± 4.7 | F | Zhou et al. (2016) |
| Cenozoic paleopoles for the Lhasa Terrane (29.5°N, 91.0°E) | ||||||||||||
| LZZV1 | Linzizong Gp, volcanic rocks | Linzhou | 54 ± 6 | 29.9 | 91.1 | 8 (46) | 71.5 | 300.1 | 6.4/11.9 | 13.0 ± 6.4 | F, D | Achache et al. (1984) |
| LZZT | Linzizong, Gp, tuff | Mendui | ∼55 | 30.1 | 90.9 | 14 (99) | 73.6 | 274.3 | 7.3 | 13.1 ± 7.3 | F, D | Sun et al. (2010) |
| PNT | Pana Fm., tuff | Linzhou | 41.5 ± 1.5 | 30 | 91.2 | 9 (76) | 87.1 | 82.6 | 5.7 | 32.4 ± 5.7 | F | Tan et al. (2010) |
| LZZV2 | Linzizong Gp, volcanic rocks | Linzhou | 62 ± 2 | 30 | 91.2 | 20 | 66.4 | 262.5 | 6.3 | 6.1 ± 6.3 | F, D | Chen et al. (2010); Chen et al. (2014) |
| LZZV3 | Linzizong Gp, volcanic rocks | Linzhou | 55 ± 5 | 30 | 91.2 | 13 | 69.7 | 268.6 | 6.3 | 9.2 ± 6.3 | F, D | Chen et al. (2010); Chen et al. (2014) |
| LZZV4 | Linzizong Gp, volcanic rocks | Linzhou | 47 ± 3 | 30 | 91.2 | 18 | 69.1 | 234.2 | 5.6 | 12.2 ± 5.6 | F, D | Chen et al. (2010); Chen et al. (2014) |
| DykeL | Linzizong Gp, dykes | Linzhou | ∼53 | 30 | 91.1 | 9 (63) | 72 | 225.5 | 5.8 | 16.2 ± 5.8 | D | Liebke et al. (2010) |
| LZZV3 | Linzizong Gp, volcanic rocks | Linzhou | 50.5 ± 3.5 | 30 | 91.1 | 24 (195) | 77.6 | 211.3 | 5.0 | 22.7 ± 5.0 | F, D | Dupont-Nibet et al. (2010) |
| LZVS | Linzizong Gp, volcanics and sediments | Linzhou | 52 ± 8 | 30 | 91.2 | 23 (148) | 70.6 | 281 | 5.3 | 10.4 ± 5.3 | F, D | Chen et al. (2010) |
| PVS | Pana Fm., volcanics and sediments | Linzhou | 48.5 ± 5.5 | 30 | 91.2 | (119) | 68.4 | 243 | 1.9 | 10.1 ± 1.9 | D | Huang et al. (2013) |
| CJD | Upper Cuojiangding Gp, sediments | Zhongba | 50 ± 16 | 29.9 | 84.3 | (62) | 78 | 329 | 5.9 | 22.7 ± 5.9 | F | Meng et al. (2012) |
| DZV2 | Member II, Dianzhong Fm., volcanics | Linzhou | 62 ± 2 | 30 | 91.2 | 35 (228) | 65.8 | 254.1 | 4.4 | 6.2 ± 4.4 | C | Chen et al. (2010); Chen et al. (2014); Huang et al. (2015); Yi et al. (2017) |
| Cretaceous-Cenozoic paleopoles for the Tethyan-Himalayan Terrane (29.5°N, 91.0°E) | ||||||||||||
| ZP1 | Zongpu Fm., limestone | Gamba, Duela | 59 ± 4 | 28.3 | 88.5 | 14 (113) | 65.4 | 277.6 | 3.8/7.6 | 5.0 ± 3.8 | F | Patzelt et al. (1996) |
| ZP2 | Zongpu Fm., marine sediments | Gamba | 60.5 ± 1.5 | 28.3 | 88.5 | 18 (171) | 67.3 | 266.3 | 3.5 | 6.9 ± 3.5 | F | Yi et al. (2011) |
| ZP3 | Zongpu Fm., marine sediments | Gamba | 57.5 ± 1.5 | 28.3 | 88.5 | 14 (141) | 71.6 | 277.8 | 2.5 | 11.2 ± 2.5 | F | Yi et al. (2011) |
| ZS | Zongshan Fm., limestone | Gamba, Duela | 68 ± 3 | 28.3 | 88.5 | 14 (156) | 55.8 | 261.4 | 4.4/8.6 | −4.3 ± 4.4 | F | Patzelt et al. (1996) |
| 28 | 89.2 | |||||||||||
| SM | Sangdanlin and Mubala sections | Saga | 60.85 ± 1.65 | 29.3 | 85.3 | (86) | 74 | 278.5 | 2.5 | 13.6 ± 2.5 | F, R | Yuan et al. (2020) |
| CAB | Cailangba A and B sections | Gyangze | 75.1 ± 1.1 | 28.9 | 89.2 | (127) | 40.8 | 256.3 | 1.8 | −18.4 ± 1.8 | R | Yuan et al. (2020) |
| SD | Sangdanlin Fm., marine deposits | Zhongba | 107.4 ± 13.5 | 29.7 | 84 | 12 (53) | 25 | 285.7 | 4.8/7.1 | −33.7 ± 4.8 | R | Qin et al. (2019) |
| SAXV | Sangxiu Fm., volcanic rocks | Langkazi | 129.5 ± 5.5 | 28.8 | 91.3 | 26 (216) | −5.9 | 308 | 6.1 | −47.9 ± 6.1 | F, R | Ma et al. (2016) |
| LKV | Lakang Fm., volcanic rocks | Cuona | 132.5 ± 1.5 | 28.1 | 92.4 | 31 (225) | −26.8 | 315.2 | 5.7 | −51.2 ± 5.7 | F, R | Yang et al. (2015) |
| ZLWM | Zhela and Weimei formations, volcanic rocks | Zhuode | 136.5 ± 1.5 | 28.9 | 91.3 | 31(219) | 0.9 | 293.4 | 7 | −52.8 ± 7.0 | F,R | Bian et al. (2019) |
| TDS | Thakkhola-Dzong Fm., sediments | Dzong | ∼118 | 28.8 | 83.8 | (95) | 12 | 289 | 6.0/7.5 | −45.0 ± 6.0 | — | Klootwijk and Bingham (1980) |
| Cretaceous paleopoles for the Indian shield (29.5°N, 91.0°E) | ||||||||||||
| RT1 | Rajmahal Traps, volcanic rocks | Rajmahal Traps | 117.5 ± 0.5 | 24.2–25.3 | 87.4–87.8 | 25 (158) | 7 | 297 | 4.5/6 | −45.8 ± 4.5 | D | Klootwijk, (1971) |
| RT2 | Rajmahal Traps, volcanic rocks | Rajmahal Traps | 117.5 ± 0.5 | 24.2–25.3 | 87.4–87.8 | 34 (120) | 9.4 | 296.6 | 3.0/3.7 | −43.9 ± 3.0 | D | Rao and Rao (1996) |
Summary of Cretaceous and Early Cenozoic paleomagnetic poles from the Lhasa and Tethyan-Himalayan (two are from interior of Indian craton) terranes.
In the original article, there was a mistake in Figure 10 as published. The selected reference site appearing in the top-right corner of the figure should read “Reference site (29.5°N, 91.0°E)” instead of “Reference site: 29.7°N, 91.0°E.” The corrected Figure 10 appears below.
FIGURE 10
In the original article, the reference for Li Z. et al. (2017) was incorrectly written as “Li, Z., Ding, L., Song, P., Fu, J., and Yue, Y. (2017d). Paleomagnetic Constraints on the Paleolatitude of the Lhasa Block during the Early Cretaceous: Implications for the Onset of India-Asia Collision and Latitudinal Shortening Estimates across Tibet and Stable Asia. Gondwana Res. 41, 352–372. doi: 10.1016j.gr.2015.05.013.” Instead, it should be “Li, Z., Ding, L., Song, P., Fu, J., and Yue, Y. (2017). Paleomagnetic Constraints on the Paleolatitude of the Lhasa Block during the Early Cretaceous: Implications for the Onset of India-Asia Collision and Latitudinal Shortening Estimates across Tibet and Stable Asia. Gondwana Res. 41, 352–372. doi: 10.1016/j.gr.2015.05.013.”
In the original article, the reference for Qasim et al. (2018) was not cited. The citation has now been inserted in Section 8 Discussion, “Sub-section 8.2 Implications to Timing of Initial India-Asia Collision,” Paragraph 14:
“Recently, scientists have studied the timing of initial India-Asia collision from the perspectives of biostratigraphic constraints and sedimentary records (DeCelles et al., 2014; Wu et al., 2014; Hu et al., 2015, 2016a; Qasim et al., 2018; Wei et al., 2020).”
In the original article, there was an error in the text. The authors mistakenly wrote “7,100 ± 530 km” and “6,400 ± 550 km” as “7,100 ± 540 km” and “6,400 ± 560 km”. A correction has been made to the Section Highlights, point 3:
“The Neo-Tethys Ocean reached its maximum N-S width of 7,100 ± 530 km at ∼132 Ma and shrank to 6,400 ± 550 km at ∼115 Ma.”
In the original article, there was an error. The authors mistakenly wrote “lower” as “higher.” A correction has been made to Section 5 Magnetic Mineralogy and Petrography, “Sub-section 5.1.2 Temperature Dependence of the Magnetic Susceptibility Measurements,” Paragraph 1:
“Moreover, all samples show that the heating curves are significantly lower than the cooling curves.”
In the original article, there was an error. The authors wrongly cited the reference citation of Li et al. (2016). A correction has been made to Section 8 Discussion, “Sub-section 8.2 Implications to Timing of Initial India-Asia Collision,” Paragraph 12:
“Thus, given the originality of this batch of paleomagnetic data set, it is clear that we also demonstrate the robustness of the previously obtained paleomagnetic results from the Duoni Fm. volcano-sedimentary rocks (Li Z. et al., 2017).”
The authors apologize for these errors and state that this does not change the scientific conclusions of the article in any way. The original article has been updated.
Statements
Publisher’s note
All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.
Reference
1
LiZ.DingL.SongP.FuJ.YueY. (2017). Paleomagnetic Constraints on the Paleolatitude of the Lhasa Block during the Early Cretaceous: Implications for the Onset of India-Asia Collision and Latitudinal Shortening Estimates across Tibet and Stable Asia. Gondwana Res.41, 352–372. 10.1016/j.gr.2015.05.013
Summary
Keywords
Lhasa terrane, India-Asia collision, Neo-Tethys ocean, paleolatitude, geochronology, intracontinental crustal shortening
Citation
Li Z, Ding L, Laskowski AK, Burke WB, Chen Y, Song P, Yue Y and Xie J (2022) Corrigendum: New Paleomagnetic Constraints on the Early Cretaceous Paleolatitude of the Lhasa Terrane (Tibet). Front. Earth Sci. 10:953708. doi: 10.3389/feart.2022.953708
Received
26 May 2022
Accepted
09 June 2022
Published
11 July 2022
Volume
10 - 2022
Edited and reviewed by
Derek Keir, University of Southampton, United Kingdom
Updates
Copyright
© 2022 Li, Ding, Laskowski, Burke, Chen, Song, Yue and Xie.
This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
*Correspondence: Zhenyu Li, lizy@itpcas.ac.cn
This article was submitted to Structural Geology and Tectonics, a section of the journal Frontiers in Earth Science
Disclaimer
All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.