Figure 2 (IMAGE)

Science China Press

Figure 2

Caption

(a) Relationships between stratal completeness and different depositional settings (water depths), climates and Rmax. (b) Four types of tectonic subsidence patterns. (c) Relationship between stratal completeness for a simulation using a 20 kyr time-step and different tectonic subsidence patterns.

Credit

©Science China Press

Usage Restrictions

Use with credit.

License

Licensed content

Disclaimer: AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert system.