1. Plate boundaries are always associated with a specific basin, which can evolve through a variety of tectonic, structural, and depositional processes. a) Discuss the connection between plate tectonics and the formation of the Sawaring basin b) Explain the characteristics of the proposed depositional environment and relate with the sedimentation process.
1. Plate boundaries are always associated with a specific basin, which can evolve through a variety of tectonic, structural, and depositional processes. a) Discuss the connection between plate tectonics and the formation of the Sawaring basin b) Explain the characteristics of the proposed depositional environment and relate with the sedimentation process.
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Question
1. Plate boundaries are always associated with a specific basin, which can evolve through a variety of tectonic, structural, and depositional processes.
a) Discuss the connection between plate tectonics and the formation of the Sawaring basin
b) Explain the characteristics of the proposed depositional environment and relate with the sedimentation process.
![Late Cretaceous
volcanie - plutonie
are
rifted continental block
accretionary foreare
complex
basin
turbidites
Estretching -->
Late Eocene
foreland Cyele I carbonate
depressicn
reefs
foesil velcaric
submerged
continent
on uplifted
tarbidites
uplift
are
SOUTH CHINA SEA
aubsidence
Oligocene - Miocene
S. C. S.
+ PLATFORM- Sawaring Basin
RAJANG GROUP >
Lupar Line
shef
progradation
SOUTH CHNA SEA
PRE-CRETACEOUS
BASEMENT
uplift](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2Fb545946b-6295-415d-a712-d16815d3a2e8%2Febbe862c-e3e4-4994-9770-624312d7d58d%2Fgf0kimu4_processed.png&w=3840&q=75)
Transcribed Image Text:Late Cretaceous
volcanie - plutonie
are
rifted continental block
accretionary foreare
complex
basin
turbidites
Estretching -->
Late Eocene
foreland Cyele I carbonate
depressicn
reefs
foesil velcaric
submerged
continent
on uplifted
tarbidites
uplift
are
SOUTH CHINA SEA
aubsidence
Oligocene - Miocene
S. C. S.
+ PLATFORM- Sawaring Basin
RAJANG GROUP >
Lupar Line
shef
progradation
SOUTH CHNA SEA
PRE-CRETACEOUS
BASEMENT
uplift
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