The podiform chromite deposits exhibit cumulate texture and occur in thehighly-depleted pyrolite of ophiolites.
文章提出豆荚状铬铁矿床不是上地幔局部熔融后的残余物，而是亏损地幔又经部分熔融形成的熔体发生液相不混熔，导致硅酸盐岩浆和富铬矿浆的形成。
Osmium isotope composition of komatiites and podiform chromitites: implications for petrogenesis;
科马提岩和豆荚状铬铁矿的Os同位素组成及其成因意义
Review on Platinum-group elements geochemistry of podiform chromitites;
豆荚状铬铁矿铂族元素地球化学研究进展
Thousands of ore samples from the Neoarchean podiform chromitite in Zunhua have been checked in detail, to identify high-temperature deformation structures, including banded, flattened antinodular textures, mylonitic foliation and so on.
豆荚状铬铁矿是蛇绿岩套地幔构造岩中特征的矿产,其矿石发育丰富的岩浆活动-高温变形结构构造类型,豆荚状铬铁矿高温下仍具有稳定的物理化学特性,对认识大洋上地幔扩张、横向运移具有重要指示意义。