We appreciate your helpful and constructive comments. We give our response below. Note that we will upload our revised manuscript after we address all referees’ comments. Thus we have answered your comments by describing how we revised the manuscript.

For the evolutionary process analysis part in the second paragraph of Section 4.2, we have more carefully reviewed the relevant materials, revised the relevant expressions and added references to the papers. Examples (a), (b), (c), and (e) are now supported by relevant papers. However, examples (d) and (f) are not as well-known as the other examples, and we still cannot find papers on the evolutionary process of this relic, so we can only study the evolutionary process of these two examples from the perspective of the evolutionary process of typical tectonic types. We know that (d) and (f) are typical angular unconformity and magmatic vein unconformity according to the descriptions on the source website and Wikipedia, so we conducted experiments on (d) and (f) according to the evolution of these two types of structures. Below is the anticipated revision:

“(a) The Piqiang Fault is on the northwest side of the Bachu Fault Zone and is connected to the Bachu Uplift in the south. Because of the uplift in the south, the stratigraphy of the area shown tends to dip to the north of the strike-slip fault (Turner et al., 2011). (b) This is a partial fold, but with erosion of relatively weak parts on both sides. The harder sandstone in the interior being cut into the ridge while the weaker shale around it is eroded (Bellahsen et al., 2005). (c) According to the description of the source, it is an igneous intrusion cut by a pegmatite dyke, which in turn is cut by a dolerite dyke, and that stratigraphic tilting occurred before the intrusion began. (d) Is a typical angular unconformity that began when the underlying strata were formed, which were then folded by crustal movement before finally being eroded and redeposited to form the overlying new strata. (e) This feature is a symmetrical and deeply eroded geodome. The circular distribution of ridges and valleys is interpreted to have been formed by differential erosion of alternating hard and soft rock layers uplifted as a dome by underlying Cretaceous alkaline igneous complexes (Matton et al., 2005). (f) This feature was formed by the superposition of a dike and an unconformity; the dike occurred first, according to the image, and then the unconformity followed.”