2 research outputs found
Supplemental Material: Subduction erosion revealed by exhumed lower arc crustal rocks in an accretionary complex, northeastern China
Figures S1–S14, Tables S1–S10, and methods.  </p
Supplemental Material: Subduction polarity reversal facilitated by plate coupling during arc-continent collision: Evidence from the Western Kunlun orogenic belt, northwest Tibetan Plateau
Materials and methods, Figures S1–S6, and Tables S1–S7.  </p