Seahorses like to live in shallow waters amongst the seaweed and eelgrass.

海马喜欢住在海藻或鳗草丛中的浅海。

Sublittoral 1. (neritic) The marine zone extending from low tide to a depth of about 200m, usually to the edge of the continental shelf.

(浅海的)由低潮延伸至两百米深处的海区，邻大陆架的边缘。

Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.

原岩形成于具有基性火山作用的活动大陆边缘滨海-浅海环境。经过太古的区域高角闪岩相变质作用，形成孔兹岩系。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据地声界面波的相关理论,采用时域有限差法立浅海沉积层中界面波传播模型。

In the paralic zone .there are ample oil and gas resources, moreover, it is the important mothball area and reliver of oil and gas industry to increase reserves and enhance output.

作为滩浅海的滨海地带,具有丰富的油气资源,是目前油气工业增储上产的重要后备区和接替区。

Seahorses like to live in shallow waters amongst the seaweed and eelgrass.

海马喜欢住在海藻或鳗草丛中的浅海。

Sublittoral 1. (neritic) The marine zone extending from low tide to a depth of about 200m, usually to the edge of the continental shelf.

(浅海的)由低潮延伸至两百米深处的海区，通常毗邻大陆架的。

Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.

岩形成于具有基性火山作的活动大陆滨海-浅海环境。经过太古的区域高角闪岩相变质作，形成孔兹岩系。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据地声界面波的相关理,时域有限差分法建立浅海沉积层中界面波传播模型。

In the paralic zone .there are ample oil and gas resources, moreover, it is the important mothball area and reliver of oil and gas industry to increase reserves and enhance output.

作为滩浅海的滨海地带,具有丰富的油气资源,是目前油气工业增储上产的重要后备区和接替区。

Seahorses like to live in shallow waters amongst the seaweed and eelgrass.

海马喜欢住在海藻或鳗草丛的浅海。

Sublittoral 1. (neritic) The marine zone extending from low tide to a depth of about 200m, usually to the edge of the continental shelf.

(浅海的)由低潮延伸至两处的海区，通常毗邻大陆架的边缘。

Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.

原岩形成于具有基性火山作用的活动大陆边缘滨海-浅海环境。经过太古的区域高角闪岩相变质作用，形成孔兹岩系。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据地声界面波的相关理论,采用时域有限差分法建立浅海沉界面波传播模型。

In the paralic zone .there are ample oil and gas resources, moreover, it is the important mothball area and reliver of oil and gas industry to increase reserves and enhance output.

作为滩浅海的滨海地带,具有丰富的油气资源,是目前油气工业增储上产的重要后备区和接替区。

Seahorses like to live in shallow waters amongst the seaweed and eelgrass.

海马喜欢住在海藻或鳗草丛中浅海。

Sublittoral 1. (neritic) The marine zone extending from low tide to a depth of about 200m, usually to the edge of the continental shelf.

(浅海)由低潮延伸至两百米深处海区，通常毗邻大陆缘。

Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.

原岩形成于具有基性火山作活动大陆缘滨海-浅海环境。经过太古区高角闪岩相变质作，形成孔兹岩系。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据地声界面波相关理论,采有限差分法建立浅海沉积层中界面波传播模型。

In the paralic zone .there are ample oil and gas resources, moreover, it is the important mothball area and reliver of oil and gas industry to increase reserves and enhance output.

作为滩浅海滨海地带,具有丰富油气资源,是目前油气工业增储上产重要后备区和接替区。

Seahorses like to live in shallow waters amongst the seaweed and eelgrass.

海马喜欢住在海藻或鳗草丛中的浅海。

Sublittoral 1. (neritic) The marine zone extending from low tide to a depth of about 200m, usually to the edge of the continental shelf.

(浅海的)由低潮延伸至两百米深处的海区，通常毗邻大陆架的边缘。

Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.

原岩形成于具有基性火山作用的活动大陆边缘滨海-浅海环境。经过太古的区域高角闪岩相变质作用，形成孔兹岩系。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据地声界面波的相关理论,采用时域有限差分法建立浅海沉积层中界面波传播模型。

In the paralic zone .there are ample oil and gas resources, moreover, it is the important mothball area and reliver of oil and gas industry to increase reserves and enhance output.

作为滩浅海的滨海地带,具有丰富的资源,是目前业增储上产的重要后备区和接替区。

Seahorses like to live in shallow waters amongst the seaweed and eelgrass.

海马喜欢住在海藻或鳗草丛中的浅海。

Sublittoral 1. (neritic) The marine zone extending from low tide to a depth of about 200m, usually to the edge of the continental shelf.

(浅海的)由低潮延伸至两百米深处的海区，通常毗邻大陆架的边缘。

Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.

原岩形成于具有基性火山作用的活动大陆边缘滨海-浅海环境。经过太古的区域高角闪岩相变质作用，形成孔兹岩系。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据地声界面波的相关理论,采用时域有限差分法建立浅海沉积层中界面波传播模型。

In the paralic zone .there are ample oil and gas resources, moreover, it is the important mothball area and reliver of oil and gas industry to increase reserves and enhance output.

作为滩浅海的滨海地带,具有丰富的油气资源,是目前油气工业增的重要后备区和接替区。

Seahorses like to live in shallow waters amongst the seaweed and eelgrass.

海马喜欢住在海藻或鳗草丛中的浅海。

Sublittoral 1. (neritic) The marine zone extending from low tide to a depth of about 200m, usually to the edge of the continental shelf.

(浅海的)由低潮延伸至两百米深处的海区，通常毗邻的边缘。

Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.

原岩形成于具有基性火山作用的活动边缘滨海-浅海环境。经过太古的区高角闪岩相变质作用，形成孔兹岩系。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据地声界面波的相关理论,采用时有差分法建立浅海沉积层中界面波传播模型。

In the paralic zone .there are ample oil and gas resources, moreover, it is the important mothball area and reliver of oil and gas industry to increase reserves and enhance output.

作为滩浅海的滨海地带,具有丰富的油气资源,是目前油气工业增储上产的重要后备区和接替区。

Seahorses like to live in shallow waters amongst the seaweed and eelgrass.

海马喜欢住在海藻或鳗草丛中的浅海。

Sublittoral 1. (neritic) The marine zone extending from low tide to a depth of about 200m, usually to the edge of the continental shelf.

(浅海的)由低潮延伸至两百米深处的海区，通常毗邻大陆架的边缘。

Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.

原岩形成于具有基作用的活动大陆边缘滨海-浅海环境。经过太古的区域高角闪岩相变质作用，形成孔兹岩系。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根界面波的相关理论,采用时域有限差分法建立浅海沉积层中界面波传播模型。

In the paralic zone .there are ample oil and gas resources, moreover, it is the important mothball area and reliver of oil and gas industry to increase reserves and enhance output.

作为滩浅海的滨海带,具有丰富的油气资源,是目前油气工业增储上产的重要后备区和接替区。

Seahorses like to live in shallow waters amongst the seaweed and eelgrass.

马喜欢住在藻或鳗草丛中的。

Sublittoral 1. (neritic) The marine zone extending from low tide to a depth of about 200m, usually to the edge of the continental shelf.

(的)由低潮延伸至两百米深处的区，通常毗邻大陆架的边缘。

Its original rock is sedimented in the environment of active epicontinent-seaboard with basic volcanism, and become khondalite series through the Archean regional high-amphibolite facies metamorphism.

原岩形成于具有基性火山作用的活动大陆边缘滨-环境。经过太古的区域高角闪岩相变质作用，形成孔兹岩系。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据地声界面波的相关理论,采用时域有限差分法建立沉积层中界面波传播模型。

In the paralic zone .there are ample oil and gas resources, moreover, it is the important mothball area and reliver of oil and gas industry to increase reserves and enhance output.

作为的滨地带,具有丰富的油气资源,是目前油气工业增储上产的重要后备区和接替区。