2
Abb. 7.1: aus: Bahlburg & Breitkreuz (1998) Abb. 7.2: Plot of mean flow velocity against median sediment size (both standardized to 10°C water temperature) for a mean flow depth of 0.25-0.40 m to show the existence fields of bedforms. After Southard (1991). aus: Allen (1997) Abb. 7.3: aus: Allen (1997) Abb. 7.4: aus: Allen (1997) B = k*h/μ*U k = Scherfestigkeit Abb. 7.5: aus: Allen (1997) SEDI 07

SEDI 07 - TU Bergakademie Freiberg · Abb. 7.2: Plot of mean flow velocity against median sediment size (both standardized to 10°C water temperature) for a mean flow depth of 0.25-0.40

  • Upload
    others

  • View
    3

  • Download
    0

Embed Size (px)

Citation preview

Page 1: SEDI 07 - TU Bergakademie Freiberg · Abb. 7.2: Plot of mean flow velocity against median sediment size (both standardized to 10°C water temperature) for a mean flow depth of 0.25-0.40

Abb. 7.1: aus: Bahlburg & Breitkreuz (1998)

Abb. 7.2: Plot of mean flow velocity against median sediment size (both standardized to 10°C water temperature) for a mean flow depth of 0.25-0.40 mto show the existence fields of bedforms. After Southard (1991).aus: Allen (1997)

Abb. 7.3:

aus: Allen (1997)

Abb. 7.4:

aus: Allen (1997)

B = k*h/µ*U

k = Scherfestigkeit

Abb. 7.5:

aus: Allen (1997)

SEDI 07

Page 2: SEDI 07 - TU Bergakademie Freiberg · Abb. 7.2: Plot of mean flow velocity against median sediment size (both standardized to 10°C water temperature) for a mean flow depth of 0.25-0.40

Abb. 8.1:

aus: Leeder (1982)

Abb. 8.2:

aus: Nichols (1999)

Abb. 8.3:

aus: Prothero & Schwab (1996)

Abb.8.4: Proximal to distal changes in the deposits formed by a turbidity current.aus: Nichols (1999).

Abb. 8.5:

Abb. 8.6:aus: Nichols (1999) SEDI 08