scholarly journals Seismological evidence for the earliest global subduction network at 2 Ga ago

2020 ◽  
Vol 6 (32) ◽  
pp. eabc5491 ◽  
Author(s):  
Bo Wan ◽  
Xusong Yang ◽  
Xiaobo Tian ◽  
Huaiyu Yuan ◽  
Uwe Kirscher ◽  
...  

The earliest evidence for subduction, which could have been localized, does not signify when plate tectonics became a global phenomenon. To test the antiquity of global subduction, we investigated Paleoproterozoic time, for which seismic evidence is available from multiple continents. We used a new high-density seismic array in North China to image the crustal structure that exhibits a dipping Moho bearing close resemblance to that of the modern Himalaya. The relict collisional zone is Paleoproterozoic in age and implies subduction operating at least as early as ~2 billion years (Ga) ago. Seismic evidence of subduction from six continents at this age is interpreted as the oldest evidence of global plate tectonics. The sutures identified can be linked in a plate network that resulted in the assembly of Nuna, likely Earth’s first supercontinent. Global subduction by ~2 Ga ago can explain why secular planetary cooling was not appreciable until Proterozoic time.


2017 ◽  
Vol 480 ◽  
pp. 33-41 ◽  
Author(s):  
Zhen Liu ◽  
Xiaobo Tian ◽  
Rui Gao ◽  
Gaochun Wang ◽  
Zhenbo Wu ◽  
...  


2021 ◽  
pp. 229012
Author(s):  
Xuelei Li ◽  
Zhiwei Li ◽  
Yufei Xi ◽  
Yutao Shi ◽  
Xiangteng Wang ◽  
...  


2014 ◽  
Vol 81 ◽  
pp. 53-64 ◽  
Author(s):  
Wenliang Jiang ◽  
Xin Wang ◽  
Tian Tian ◽  
Jingfa Zhang ◽  
Donglei Wang


2019 ◽  
Vol 185 ◽  
pp. 104045 ◽  
Author(s):  
Feng Bao ◽  
Zhiwei Li ◽  
Baofeng Tian ◽  
Liaoliang Wang ◽  
Guanghong Tu


2019 ◽  
Vol 7 (4) ◽  
pp. T857-T867 ◽  
Author(s):  
Mei Liu ◽  
Irina Filina ◽  
Paul Mann

We have investigated the crustal structure of a 400 km wide zone of thinned continental crust in the northeastern Gulf of Mexico (GOM) using gravity and magnetic modeling along two deeply penetrated seismic transects. Using this approach, we identify two zones of prominent, southward-dipping reflectors associated with 7–10 km thick, dense, and highly magnetic material. Previous workers have interpreted the zones as either coarse clastic redbeds of Mesozoic age that are tilted within half-grabens or seaward-dipping reflectors of magmatic origin. Both seismic reflection lines reveal a 10 km thick and 67 km wide northern zone of high density near the Florida coastline beneath the Apalachicola rift (AR). The southern zone of high density occurs 70 km to the south in the deepwater central GOM along the northern flank of the marginal rift, a 48 km wide, southeast-trending structure of inferred Late Jurassic age that is filled by 3 km of low-density and low-magnetic susceptibility sediments including complexly deformed salt deposits. We propose that these two subparallel rifts and their associated magmatic belts formed in the following sequence: (1) AR formed during Triassic-early Jurassic (210–163 Ma) phase 1 of diffuse continental stretching and was partially infilled on its northern edge by southward-dipping volcanic flows; and (2) the similarly southward-dipping southern magmatic zone formed adjacent to the marginal rift during the early phase 2 of late Jurassic (161–153 Ma) rifting of the GOM continental extension; this southern area of SDR formation immediately preceded the formation of the adjacent oceanic crust that separated the rift-related evaporates into the northern and southern GOM. Our integrated approach combining 2D seismic, gravity, and magnetic data sets results in a more confident delineation of these deep crustal features than from seismic data alone.



2014 ◽  
Vol 387 ◽  
pp. 198-211 ◽  
Author(s):  
Chun-Yong Wang ◽  
E. Sandvol ◽  
L. Zhu ◽  
Hai Lou ◽  
Zhixiang Yao ◽  
...  




2018 ◽  
Vol 31 (5-6) ◽  
pp. 242-251
Author(s):  
Gaochun Wang ◽  
◽  
Xiaobo Tian ◽  
Lianglei Guo ◽  
Jiayong Yan ◽  
...  


2009 ◽  
Vol 54 (19) ◽  
pp. 3354-3366 ◽  
Author(s):  
RiXiang Zhu ◽  
TianYu Zheng


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