An olistostrome is a sedimentary deposit composed of a chaotic mass of heterogeneous material, such as blocks and mud, known as olistoliths, that accumulates as a semifluid body by submarine gravity sliding or slumping of the unconsolidated sediments.

2016年11月1日 · Olistostromes represent ancient examples of modern submarine MTDs and MTCs. Olistostromes are significant markers of tectonic and climatic events worldwide. Olistostromes (sedimentary mélanges) represent the products of ancient submarine mass transport processes.

2016年11月1日 · Olistostromes (sedimentary mélanges) represent the products of ancient submarine mass transport processes.

The terms olistostrome and olistolith have been introduced by G. Flores (4 th World Petroleum Congress, Rome, 1955) to indicate either mass-transported bodies with a chaotic block-in-matrix fabric, or single slide blocks, intercalated between layered sequences in …

Olistostromes (sedimentary mélanges) represent the products of ancient submarine mass transport processes.

2010年1月1日 · Olistostrome and sedimentary mélange are two synonymous genetic terms referring to the “fossil” products of ancient submarine mass‐transport processes exhumed in orogenic belts.

This unique terrane is an olistostrome that was shed eastward by listric faulting from the east side of the migrating Antler orogenic forebulge in Late Devonian (early Famennian, ca. 373 Ma) time.

The terms olistostrome and olistolith have been introduced by G. Flores (4th World Petroleum Congress, Rome, 1955) to indicate either mass-transported bodies with a chaotic block-in-matrix fabric, or single slide blocks, intercalated between layered sequences in …

This unique terrane is an olistostrome that was shed eastward by listric faulting from the east side of the migrating Antler orogenic forebulge in Late Devonian (ea

Olistostrome A sedimentary deposit consisting of a chaotic mass of intimately mixed heterogeneous materials (such as blocks and muds) that accumulated as a semi-fluid body by submarine gravity sliding or slumping of unconsolidated sediments.