在位置 0 处没有任何行。 镇旬盆地南缘淋湘金矿床流体来源及其成因探讨：C-H-O-Fe同位素、磷灰石裂变径迹的证据-Discussion on fluid source and genesis of Linxiang gold deposit in southern margin of Zhenshi Basin: evidence from C-H-O isotope and apatite fission track