Gurmeet singh Asked a Question
November 28, 2020 11:30 pmpts 30 pts
TOundness. us Generally the elongation quotient is maximum in metamorphic rocks, less 9 rocks and very less in sedimentary rocks. Thus when the source rock is of metamo origin, the sphericity of the clastic grains is not that much pronounced. ) Packing It is the manner of aggregation of sedimentary grains, which are held together in
  • 1 Answer(s)
  • 0 Likes
  • 1 Comments
  • Shares
  • Rahul kumar Best Answer
    Metamorphic rocks commonly form under differential stress (unequal stress from different directions) condition. As a result of differential stress, the mineral grains show elongate...
    Show more
    Likes(1) Reply(0)
Head Office :
MPA 44, 2nd floor, Rangbari Main Road,
Mahaveer Nagar II, Kota (Raj.) – 324005

Corporate Office:
212, F-1, 2nd Floor, Evershine Tower,
Amrapali Marg,
Vaishali Nagar, Jaipur (Raj.) – 302021

Mail: info@eduncle.com
All Rights Reserved © Eduncle.com